Abstract

The occurrence of thermal convection in groundwater could significantly change groundwater flows, and this phenomena could also alter solute transport. In the case of a shallow groundwater, thermal convection might affect the surface water quality because it directly interacts with surface waters such as lakes and marshes. Hence, understanding the conditions that induce thermal convection is important for groundwater management. In this study, the conditions for the onset and decay of thermal convection in a flowing shallow groundwater are investigated by conducting numerical experiments. Through the computational analysis using the attractor reconstruction technique, three flow regime types were found, showing that not only the Rayleigh number, which is a well-known influential factor, but also the groundwater flow rate affects the flow regime.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call