TY - JOUR
T1 - Anomalous Dispersion in Pore-Scale Simulations of Two-Phase Flow
AU - Triadis, Dimetre
AU - Jiang, Fei
AU - Bolster, Diogo
N1 - Funding Information:
Acknowledgements This research was made possible by a Kyushu University, International Institute for Carbon Neutral Energy Research (I2CNER), Competitive Funding Initiative on Applied Math for Energy Project Grant. We would also like to express thanks for financial support via NSF Grants EAR-1351625, EAR-1446236 and CBET-1803989, as well as a JSPS Grant-in-Aid for Young Scientists (16K18331).
Publisher Copyright:
© 2018, Springer Nature B.V.
PY - 2019/1/30
Y1 - 2019/1/30
N2 - We investigate anomalous dispersion in steady-state two-phase flow though a random, artificial porous domain. A natural distribution of trapped wetting-phase fluid was obtained via two-phase lattice Boltzmann drainage simulations. To avoid spurious velocities, accurate inter-pore velocity fields were derived via additional one-phase lattice Boltzmann simulations incorporating slip boundary conditions imposed at various interfaces. The nature of the active dispersion at various timescales was subsequently studied via random walk particle tracking. For our system, results show persistent anomalous dispersion that depends strongly on the assumed molecular diffusivity and the initial positions of tracer particles. Imposing slip versus no-slip boundary conditions on fluid–fluid interfaces made no observable difference to results, indicating that observed anomalous dispersion resulted primarily from the complex flow network induced by the trapped fluid phase.
AB - We investigate anomalous dispersion in steady-state two-phase flow though a random, artificial porous domain. A natural distribution of trapped wetting-phase fluid was obtained via two-phase lattice Boltzmann drainage simulations. To avoid spurious velocities, accurate inter-pore velocity fields were derived via additional one-phase lattice Boltzmann simulations incorporating slip boundary conditions imposed at various interfaces. The nature of the active dispersion at various timescales was subsequently studied via random walk particle tracking. For our system, results show persistent anomalous dispersion that depends strongly on the assumed molecular diffusivity and the initial positions of tracer particles. Imposing slip versus no-slip boundary conditions on fluid–fluid interfaces made no observable difference to results, indicating that observed anomalous dispersion resulted primarily from the complex flow network induced by the trapped fluid phase.
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U2 - 10.1007/s11242-018-1155-6
DO - 10.1007/s11242-018-1155-6
M3 - Article
AN - SCOPUS:85054572499
SN - 0169-3913
VL - 126
SP - 337
EP - 353
JO - Transport in Porous Media
JF - Transport in Porous Media
IS - 2
ER -