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Climate Effects on Stream Nitrate Concentrations at 16 Forested Catchments in South Central Ontario
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文摘
Increased nitrate (NO3) concentrations in streamwatersdraining forested catchments are reportedly an early indicatorof nitrogen (N) saturation. Nitrate concentrations instreams draining 16 forested catchments in south centralOntario were monitored over a 16-year period, duringwhich time N bulk deposition was relatively constant (~9kg ha-1 yr-1). Mean annual NO3 concentrations instreams were both highly variable among catchments andamong years, although patterns of annual concentrationwere similar among many catchments. Coherence analysisidentified two stream groupings. Shallow soils, moderateslopes, low NO3 concentration, and a large wetland componentcharacterized the first group. The second group hadprimarily upland characteristics including deeper soils,steeper slopes, higher NO3 concentrations, and a muchsmaller wetland component. Patterns in NO3 concentrationin wetland-influenced streams appeared to be related tosummer drought and cumulative frost depth, whereas NO3concentrations in upland-draining streams appeared tobe related to both mean annual air temperature and summerdrought. Because a number of different climate parametersas well as the physical character of the catchmentsapparently influence NO3 export, NO3 concentrations instreams are not a good indicator of N saturation in thisregion.

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