| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4577467 | Journal of Hydrology | 2011 | 10 Pages |
Abstract
⺠We model particle transport in an evolving synthetic karst aquifer. ⺠The particle breakthrough time is related to the stage of karstification. ⺠The tailing is caused by flow exchange between main channels and adjacent network. ⺠When injected into a low gradient zone, particles can stay in a network for decades.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Franci Gabrovšek, Wolfgang Dreybrodt,