Mw. Williams et Ka. Tonnessen, Critical loads for inorganic nitrogen deposition in the Colorado Front Range, USA, ECOL APPL, 10(6), 2000, pp. 1648-1665
We suggest an empirical approach for determining critical loads for inorgan
ic nitrogen (N) deposition in wetfall to the central Rocky Mountains (USA).
We define "critical loads" as a deposition amount above which natural reso
urces can be negatively affected. The arithmetic average from 1992 to 1996
of annual inorganic N deposition in wetfall at the eight National Acid-Depo
sition Program (NADP) sites located at elevations >2500 m in the central Ro
cky Mountains ranged from 2.5 to 3.5 kg.ha(-1).yr(-1). In contrast, inorgan
ic N deposition was <2.5 kg.ha(-1).yr(-1) at all 23 NADP sites below 2500 m
in elevation. At the Niwot Ridge NADP site in the Colorado Front Range, a
simple linear regression of inorganic N in wetfall with time shows a signif
icant increase in deposition of inorganic N in wetfall at the rate of 0.32
kg.ha(-1).yr(-1) (r(2) = 0.62; P < 0.001, n = 13). In turn, the increasing
amount of inorganic N in wetfall is causing episodic acidification in headw
ater catchments of the Green Lakes Valley in the Colorado Front Range, with
acid-neutralizing capacity (ANC) values below 0 mu mol(c)/L in surface wat
ers during snowmelt runoff at 9-ha and 42-ha sampling sites. At present rat
es of ANC decrease, we can expect the 9-ha and 42-ha sites to become chroni
cally acidified within the next decade and the 220-ha basin of Green Lake 4
to become episodically acidified.
A synoptic survey in 1995 of 91 high-elevation lakes in the central Rocky M
ountains suggests that water quality is being affected by inorganic N in we
tfall throughout the region. Federal land managers are required to "err on
the side of protection" when assessing the amount of deposition that will a
lter ecosystem processes. However, given the political and economic ramific
ations of policy decisions, land managers are aware of the need to provide
a scientific basis for these decisions and to balance conflicting needs. To
achieve this balance and to allow for natural-resource protection, we make
a conservative recommendation that critical loads of inorganic N in wetfal
l to Class 1 areas in the central Rocky Mountains be set at 4 kg.ha(-1).yr(
-1). Target loads may be set at lower levels of inorganic N deposition in w
etfall to allow a margin of safety to protect extremely sensitive natural r
esources.