Development of the oil sands has led to increasing atmospheric N
deposition, with values as high as 17 kg N
ha-1 yr-1;
regional background levels <2 kg N ha-1
yr-1. Bogs, being ombrotrophic, may be
especially susceptible to increasing N deposition. To examine
responses to N deposition, over five years, we experimentally applied
N (as NH4NO3) to a bog
near Mariana Lakes, Alberta, at rates of 0, 5, 10, 15, 20, and 25 kg N
ha-1 yr-1, plus
controls (no water or N addition). Resin tubes filled with mixed-bed
ion exchange resin were swapped in and out at each
collection/deployment date (mid-May and mid-October of each year).
Upon collection, resins were extracted with 1M KI and analyzed for
inorganic N concentrations. Deposition of
NH4
+-N,
NO3
--N, and DIN
averaged 187 ± 11, 237 ± 13, and 426 ± 19 μg
m-2 da-1,
corresponding to 0.68 ± 0.04, 0.87 ± 0.05, and 1.55 ± 0.07 kg N
ha-1 yr-1, with
no significant differences between open and throughfall collectors for
any of the three measured parameters (p >= 0.63). Deposition of
NH4
+-N was
significantly higher during the growing season (averaging 240 μg
m-2 da-1) than
during the winter months (averaging 121 μg
m-2 da-1) (p =
0.0004), while
NO3
--N and DIN
deposition did not differ significantly between winter and summer (p =
0.06 and 0.13, respectively).