Abstract
Conventional concepts for transport in porous media assume that the heterogeneous distribution of hydraulic conductivities is the source for the contaminant temporal and spatial heavy tail. This tailing, known as anomalous or non-Fickian transport, can be captured by the β parameter in the continuous-time random walk framework. This study shows that with the increase in spatial correlation length between these heterogeneous distributions of hydraulic conductivities, the transport’s anomaly reduces; yet, the β value is unchanged, suggesting a topological component of the conductivity field, captured by the β. This finding is verified by an analysis of the solute transport, showing that the changing conductivity values have a moderate effect on the transport shape.
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This research was supported by the ISF-NSFC joint research program (Grant No. 3333/19)
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Appendix
Appendix
As stated in Method section, a parallel simulation is presented for Δ = 0.02 so to verify that a change of Δ will have no effect on the transport. As previously, we use a field of 3000 × 1200 cells from which a 300 × 120 field is taken. Unlike the previous simulation, the absolute field size is now 6 × 1.2, an order of magnitude smaller. Thus, the head difference was reduced from 100 to 10 so to maintain the same mean velocity. The dimensionless correlation length (normalized by the field length) ranges from 1 × 10–5 to 1 × 10–4, yet there are 15 cells for the low correlation length and 150 cells for the high correlation length.
The BTC fit in Fig. 5a–c and the corresponding juxtaposition in Fig. 5d–f show that the β is still persistent for the variations in correlation length, while the t2 is reducing due to the correlation length increase, as before. Moreover, the same dispersion increase can be found with an increase in correlation length. This shows the consistency of these results, mainly since the juxtaposition in Fig. 5d–f still reproduces the same slope associated with the β. At the same time, the t2 cutoff is apparent in the PDF tail dispersion. The PPF’s analysis, as the correlation length changes, shows even higher values of PPF’s spatial occurrence for varying correlation lengths of more than 60% to 85% (Fig. 6). As for the larger field, the weighted conductivity distribution for the PPFs has the same tailing as shown in Fig. 3a–c, where the backward tail follows the weighted conductivity, and the forward tail follows the unweighted distribution (Figs. 6a–c, 7)
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Edery, Y. The Effect of varying correlation lengths on Anomalous Transport. Transp Porous Med 137, 345–364 (2021). https://doi.org/10.1007/s11242-021-01563-9
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DOI: https://doi.org/10.1007/s11242-021-01563-9