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Hydraulic reversals and episodic methane emissions during drought cycles in mires

Journal Article · · Geology; (United States)
;  [1];  [2]
  1. Syracuse Univ., NY (United States)
  2. Univ. of Minnesota, Minneapolis, MN (United States)

Reversals in hydraulic head and extensive methane losses were identified during a drought cycle from changes in hydraulic-head and dissolved-methane profiles in peat, Glacial Lake Agassiz Peatlands, northern Minnesota, United States. During the summer 1990 drought, regional groundwater discharged from the mineral soil underlying the peat to raised bogs. Concentrations of dissolved CH[sub 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[sub 4]. By the summer of 1991, the severity of the drought lessened, and the upper peat column was resaturated with precipitation-derived water. Groundwater flow was then controlled by local, precipitation-driven, recharge flow systems, and the regional groundwater that was discharged affected only the peat immediately above the mineral soil-peat interface. In contrast, during the summer of 1991, concentrations of dissolved CH[sub 4] in pore water were all undersaturated with respect to 1 atm partial pressure CH[sub 4]. 23 refs., 5 figs.

DOE Contract Number:
FG02-90ER60984
OSTI ID:
7238290
Journal Information:
Geology; (United States), Journal Name: Geology; (United States) Vol. 21:3; ISSN 0091-7613; ISSN GLGYBA
Country of Publication:
United States
Language:
English