Hydraulic reversals and episodic methane emissions during drought cycles in mires

At Glacial Lake Agassiz Peatlands, Minnesota, during the summer 1990 drought, regional ground water discharged from the mineral soil underlying the peat to raised bogs. Concentrations of dissolved CH ₄ in pore water showed that much of the peat column was supersaturated with respect to a reference standard of 1 atm partial pressure CH ₄ . As the severity of the drought lessens, the upper peat column was resaturated with precipitation-derived water. Ground-water flow was then controlled by local, precipitation-driven, recharge flow systems, and the regional ground water that was discharged affected only the peat immediately above the mineral soil-peat interface. During the summer of 1991, concentrations of dissolved CH ₄ in pore water were all undersaturated with respect to 1 atm partial pressure CH ₄ . The decrease in the amount of dissolved CH ₄ in the pore water was probably caused by changes in the CH ₄ flux and degassing to the unsaturated zone and by changes in the partial pressure of gaseous CH ₄ in the peat as the peat volume increased as it resaturated. -from Authors