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CRITICAL LOADS FOR INORGANIC NITROGEN DEPOSITION IN THE COLORADO FRONT RANGE, USA
Author(s) -
Williams Mark W.,
Tonnessen Kathy A.
Publication year - 2000
Publication title -
ecological applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.864
H-Index - 213
eISSN - 1939-5582
pISSN - 1051-0761
DOI - 10.1890/1051-0761(2000)010[1648:clfind]2.0.co;2
Subject(s) - deposition (geology) , snowmelt , acid neutralizing capacity , hydrology (agriculture) , environmental science , drainage basin , surface runoff , nitrogen , acid deposition , ecology , environmental chemistry , structural basin , chemistry , geology , soil water , soil science , geography , geomorphology , biology , geotechnical engineering , cartography , organic chemistry
We suggest an empirical approach for determining critical loads for inorganic nitrogen (N) deposition in wetfall to the central Rocky Mountains (USA). We define “critical loads” as a deposition amount above which natural resources can be negatively affected. The arithmetic average from 1992 to 1996 of annual inorganic N deposition in wetfall at the eight National Acid‐Deposition Program (NADP) sites located at elevations >2500 m in the central Rocky Mountains ranged from 2.5 to 3.5 kg·ha −1 ·yr −1 . In contrast, inorganic 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 significant 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 headwater catchments of the Green Lakes Valley in the Colorado Front Range, with acid‐neutralizing capacity (ANC) values below 0 μmol c /L in surface waters during snowmelt runoff at 9‐ha and 42‐ha sampling sites. At present rates of ANC decrease, we can expect the 9‐ha and 42‐ha sites to become chronically 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 Mountains suggests that water quality is being affected by inorganic N in wetfall throughout the region. Federal land managers are required to “err on the side of protection” when assessing the amount of deposition that will alter ecosystem processes. However, given the political and economic ramifications 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 wetfall 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 wetfall to allow a margin of safety to protect extremely sensitive natural resources.