J. Kahl et al., Nitrogen and sulfur input-output budgets in the experimental and referencewatersheds, Bear Brook Watershed in Maine (BBWM), ENV MON ASS, 55(1), 1999, pp. 113-131
Dry (NH4)(2)SO4 (1,800 eq(-1) ha(-1) yr(-1)) has been applied to the wester
n of two contiguous 10 ha catchments at the Bear Brook Watershed in Maine (
BBWM) since November, 1989. The initial rapid and significant response in b
oth S and N in West Bear, compared to the reference East Bear, slowed after
three years. Annual S retention of the total experimental treatment decrea
sed from 86 to 34%, with a seven year cumulative retention of 59%. Hydrolog
y influences the export flux of S; S is retained more in dry seasons and dr
y years. The annual retention of N has decreased from 96 to 81%, with a cum
ulative retention of 82%. The export of N from the reference watershed has
declined from 178 to 23 eq(-1) ha(-1) yr(-1) during the treatment period. T
he treatment N (as NH4) initially stimulated nitrification, and caused pre-
existing N to be lost in runoff rather than the treatment N. Retention of t
he treatment N has decreased to approximately 80%. The majority of the reta
ined N is stored in the soil, but the reasons for the decreased flux from t
he reference watershed are not known.