Nitrogen Saturation in the Rocky Mountains
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文摘
Nitrogen saturation is occurring throughout high-elevation catchments of the Colorado Front Range.Annual inorganic N loading in wet deposition to theFront Range of ~4 kg ha-1 yr-1 is abouttwice thatof the Pacific States and similar to many sites in thenortheastern United States. In the last ten yearsat Niwot Ridge/Green Lakes Valley and Glacier Lakes,annual minimum concentrations of NO3- insurfacewaters during the growing season have increasedfrom below detection limits to ~10 µequiv L-1,indicatingthat these two catchments are at the threshold ofN saturation. The Loch Vale watershed is N saturated,with annual minimum concentrations of NO3-insurface waters generally above 10 µequiv L-1;annualvolume-weighted mean (VWM) concentrations of16 µequiv L-1 in surface waters are greater thanthatof ~11 µequiv L-1 NO3- inwet deposition. At thesehigh-elevation catchments, there has been a shift inecosystem dynamics from an N-limited system toan N-saturated system as a result of anthropogenicallyfixed N in wetfall and dryfall. Results from theWestern Lakes Survey component of the NationalSurface Water Survey show that N saturation is aregional problem in the Colorado Front Range, withmany lakes having (NO3-) concentrationsgreater than10 µequiv L-1. Foliar N:P ratios in bristleconepineincrease with elevation in the Colorado Front Range,indicating that at higher elevations P is translocatedfrom foliar tissue more efficiently than N and thatincreasing atmospheric deposition of N with elevationis causing a change from N limitation to P limitationin the highest-elevation bristlecone pines. Currentconcepts of critical loads need to be reconsidered sinceonly modest atmospheric loadings of N are sufficientto induce N leaching to surface waters inhigh-elevation catchments of the western UnitedStates.

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