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Chemical Fluxes from Sediments in Two Adirondack Wetlands

Effects of an Acid-Neutralization Experiment

^a Dep. of Geology, State Univ. of New York College at Cortland, Cortland, NY 13405 USA
^b Dep. of Civil and Environ. Engineering, Syracuse Univ., Syracuse, NY 13244 USA
^c Dep. of Art and Archaeology, Princeton Univ., Princeton, NJ 08544 USA

View larger version (19K): [in a new window]   Fig. 1 Location of the CaCO3–treated beaver pond (Woods Lake) and the reference beaver pond in the Adirondack Mountain region of New York

View larger version (39K): [in a new window]   Fig. 2 Time trends in SO2-4, NH+4, and Fe2+ concentrations for enclosure Experiment 1 in the reference beaver pond

View larger version (41K): [in a new window]   Fig. 3 Time trends in SO2-4, NH+4, and Fe2+ concentrations for enclosure Experiment 1 in the CaCO3–treated beaver pond

View larger version (41K): [in a new window]   Fig. 4 Time trends in acid-neutralizing capacity (ANC), dissolved organic carbon (DOC), and Ca2+ concentrations for enclosure Experiment 2 in the reference beaver pond

View larger version (38K): [in a new window]   Fig. 5 Time trends in Fe2+, H4SiO4, inorganic monomeric Al (AlIM), and organic monomeric Al (AlOM) concentrations for enclosure Experiment 2 in the reference beaver pond

View larger version (44K): [in a new window]   Fig. 6 Time trends in acid-neutralizing capacity (ANC), dissolved organic carbon (DOC), and Ca2+ concentrations for enclosure Experiment 2 in the CaCO3–treated beaver pond

View larger version (38K): [in a new window]   Fig. 7 Time trends in Fe2+, H4SiO4, inorganic monomeric Al (AlIM), and organic monomeric Al (AlOM) concentrations for enclosure Experiment 2 in the CaCO3–treated beaver pond