Hi all,
I am running coupled ATS-Alquimia-PFLOTRAN simulations of reactive transport in a 2D Arctic permafrost hillslope (a supra-permafrost aquifer with seasonal freeze-thaw). My reaction network includes aerobic respiration, fermentation, iron reduction, and methanogenesis with 10 primary species. The problem I am running into is with O2 delivery to the subsurface.
In my current setup, the only way O2 enters the subsurface is dissolved in rainfall infiltrating from the surface. When the water table drops and the active layer desaturates, no O2 enters the air-filled pores because the ATS-PFLOTRAN coupling is single-phase (aqueous only) and ATS transport PK does not handle gas-phase transport. This means the subsurface stays permanently anaerobic even during dry periods, which is not physical. In reality, atmospheric O2 should diffuse as subsurface unsaturates. And also degassing of CO2 and CH4 should happen simulataneously.
I know that standalone PFLOTRAN can handle gas-phase transport, but with ATS, as PFLOTRAN acts as a batch reactor, I don't think I can use the gas transport part. Please let me know if there are any workarounds to use that as well. I am wondering if it is possible to approximate (fake) O2 aeration/ CO2 degassing using a reaction sandbox -maybe a saturation depndent source/sink? Please let me know if anyone has done something like this or has any other workarounds.
In teh attached files, I have an example of the reactions that I am using currently along with an example ATS input file.
Thanks,
Neel.