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Norton, S.A., J.S. Kahl, I.J. Fernandez, T.A. Haines, L.E. Rustad, S.C. Nodvin, J.P. Scofield, T.C. Strickland, H.E. Erickson, Parker J. Wigington, Jr., and J.J. Lee. 1999. The Bear Brook Watershed (BBWM). Environmental Monitoring and Assessment 55:7-51.

The Bear Brook Watershed Manipulation project in Maine is a paired calibrated watershed study funded by the U.S. EPA. The research program is evaluating whole ecosystem response to elevated inputs of acidifying chemicals. The project consists of a 2.5 year calibration period (1987-1989), nine years of chemical additions of (NH4 )2SO4 (15N- and 34S-enriched for several years) to West Bear watershed (1989-1998), followed by a recovery period. The other watershed, East Bear, serves as a reference. Dosing is in six equal treatments/yr of 1800 eq SP4 and NH4/ha/yr, a 200% increase over 1988 loading (wet plus dry) for SO4 and 300% for N (wet NO3 + NH4). The experimental and reference watersheds are forested with mixed hard- and softwoods, and have thin acidic soils, areas of 10.2 and 10.7 ha, and relief of 210 m. thin till of variable composition is underlain by metasedimentary peltic rocks and calc-silicate gneiss intruded by granite dikes and sills. For the period 1987-1995, precipitation averaged 1.4 m/yr, had a mean pH of 4.5 with SO4, NO3 and NH4 concentrations of 26, 14, and 7eq/L, respectively. The nearly perennial streams draining each watershed have discharges ranging from ) (East Bear stops flowing for one to two months per year) to 150 L/sec. Prior to manipulation, East Bear and West Bear had a volume weighted annual mean pH of approximately 5.4 alkalinity = 0 to 4 eq/L, total base cations = 184 L (sea-salt corrected = 118/L), and SO4 = 100 to 111 eq/L. Nitrate ranged from 0 to 30 /L with an annul mean of 6 to 25 ; dissolved organic carbon (DOC) ranged from 1 to 7 mg/L but was typically less than 3. Episodic acidification occurred at high discharge and was caused by dilution of cations, slightly increased DOC, significantly higher NO3, and the sea-salt effect. Depressions in pH were accompanied by increases in inorganic Al. The west Bear catchment responded to the chemical additions with increased export of base cations, Al, SO4, NO3 and decreased pH, AN, and DOC. Silica remained relatively constant. Neutralization of the acidifying chemicals occurred dominantly by cation desorption and mobilization of Al.

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