Abstract
A three-dimensional model for non-reactive solute transport in physically homogeneous subsurface porous media is presented. The model involves solution of the advection-dispersion equation, which additionally considered temporally dependent dispersion. The model also account for a uniform flow field, first-order decay which is inversely proportional to the dispersion coefficient and retardation factor. Porous media with semi-infinite domain is considered. Initially, the space domain is not solute free. Analytical solutions are obtained for uniform and varying pulse-type input source conditions. The governing solute transport equation is solved analytically by employing Laplace transformation technique (LTT). The solutions are illustrated and the behavior of solute transport may be observed for different values of retardation factor, for which simpler models that account for solute adsorption through a retardation factor may yield a misleading assessment of solute transport in ‘‘hydrologically sensitive’’ subsurface environments.
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Acknowledgments
This study is a part of a postdoctoral fellowship of the author Dilip Kumar Jaiswal and gratefully acknowledges the financial assistance in the form of UGC, Dr. D. S. Kothari Postdoctoral Fellowship, New Delhi, India. In particular, we thank the editor-in-chief and the reviewers for their critical and detailed suggestions that helped to improve this manuscript substantially.
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Appendix
Appendix
The conditions (12–13) in terms of new space (η) and time (T) variables may be written as
Now, introducing a new dependent variable by the following transformation
The set of Eqs. 19–21 and 11 reduced to
Applying Laplace transformation on Eqs. 23–26, we have
Thus, the general solution of Eq. 27 may be written as
Using condition 28–29 on the above solution, we get
Thus, the particular solution in the Laplacian domain may be written as
Taking inverse Laplace transform of 31, the solution of advection-dispersion solute transport for uniform pulse-type input condition may be written in terms of \( c(x,y,z,T) \) by using Eqs. 22, 10, 8 and 6.
Similarly, Eq. 15 reduces by applying the transformations 6, 8, 10 and 22
Applying Laplace transformation on Eq. 32, we may get
Now using input condition 33 in place of 28 in the general solution 30, we get
Thus, the particular solution in the Laplacian domain may be written as
Taking inverse Laplace transform of 35, the solution of advection-dispersion solute transport for varying input conditions may be written in terms of \( c(x,y,z,T) \) by using Eqs. 22, 10, 8 and 6.
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Yadav, R.R., Jaiswal, D.K., Yadav, H.K. et al. Three-dimensional temporally dependent dispersion through porous media: analytical solution. Environ Earth Sci 65, 849–859 (2012). https://doi.org/10.1007/s12665-011-1129-2
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DOI: https://doi.org/10.1007/s12665-011-1129-2