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Saturation, Reduction, and the Formation of Iron–Manganese Concretions in the Jackson-Frazier Wetland, Oregon

^a USDA Forest Service, Pacific Northwest Research Station, 2770 Sherwood Lane, Suite 2A, Juneau, AK 99801
^b L.C. Lee and Associates, Seattle, WA 98119
^c Dep. of Crop and Soil Sci., Oregon State Univ., Corvallis, OR 97331

View larger version (36K): [in a new window]   Fig. 1. Duration of saturation (bottom) and electrode potentials (top) at depths of 100, 50, and 25 cm at Site JF1.

View larger version (39K): [in a new window]   Fig. 2. Duration of saturation (bottom) and electrode potentials (top) at depths of 100, 50, and 25 cm at Site JF2.

View larger version (37K): [in a new window]   Fig. 3. Dissolved oxygen (DO) in piezometer water at depths of 200, 100, 50, and 25 cm at Site JF1.

View larger version (33K): [in a new window]   Fig. 4. Dissolved oxygen (DO) in piezometer water at depths of 200, 100, 50, and 25 cm at Site JF2.

View larger version (36K): [in a new window]   Fig. 5. Soil temperature data at depths of 100, 50, and 25 cm at Site JF1.