Erschienen:
American Geophysical Union (AGU), 2022
Erschienen in:Geophysical Research Letters
Sprache:
Englisch
DOI:
10.1029/2021gl096280
ISSN:
0094-8276;
1944-8007
Entstehung:
Anmerkungen:
Beschreibung:
<jats:title>Abstract</jats:title><jats:p>The simultaneous presence of liquid and gas in porous media increases flow heterogeneity compared to saturated flows. However, the impact of saturation on flow and transport has so far remained unclear. The presence of gas in the pore space leads to flow reorganization. We develop a theoretical framework that captures the impact of that reorganization on pore‐scale fluid velocities. Preferential flow is distributed spatially through a backbone, and flow recirculation occurs in flow dead‐ends. We observe, and predict theoretically, that this previously identified flow structure induces a marked change in the scaling of the velocity probability density function compared to the saturated configuration and a sharp transition to strongly anomalous transport. We develop a transport model using the continuous time random walk theory that predicts advective transport dynamics for all saturation degrees. Our results provide a new modeling framework linking phase heterogeneity to flow heterogeneity in unsaturated porous media.</jats:p>