Wildfire impacts on nitrogen concentration and production from headwater streams in southern Alberta's Rocky Mountains

被引:84
作者
Bladon, Kevin D. [1 ]
Silins, Uldis [1 ]
Wagner, Michael J. [1 ]
Stone, Micheal [2 ]
Emelko, Monica B. [3 ]
Mendoza, Carl A. [4 ]
Devito, Kevin J. [5 ]
Boon, Sarah [6 ]
机构
[1] Univ Alberta, Dept Renewable Resources, Forest Hydrol Lab, Edmonton, AB T6G 2H1, Canada
[2] Univ Waterloo, Sch Planning, Fac Environm Studies, Waterloo, ON N2L 3G1, Canada
[3] Univ Waterloo, Dept Civil Engn, Waterloo, ON N2L 3G1, Canada
[4] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada
[5] Univ Alberta, Dept Biol Sci, Edmonton, AB T6G 2E9, Canada
[6] Univ Lethbridge, Dept Geog, Lethbridge, AB T1K 3M4, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.1139/X08-071
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The objective of this study was to examine initial effects of the 2003 Lost Creek wildfire (southwestern Rocky Mountains of Alberta) on concentrations and production (yield and total export) of several nitrogen (N) forms, and to explore initial recovery of these effects within the first 3 years after the fire. During the first postfire year, nitrate (NO3-), dissolved organic nitrogen (DON), and total nitrogen (TN) concentrations in severely burned watershed streams were 6.5, 4.1, and 5.3 times greater, respectively, than those in reference streams. Weaker effects were evident for concentrations of ammonium (NH4+; 1.5 times) and total particulate nitrogen (TPN; 3.0 times). A rapid decline in mean watershed concentrations and production of NO3-, DON, total dissolved nitrogen (TDN), and TN was observed from burned watersheds over the three seasons after the fire. However, elevated NO3-, TDN, and TN concentrations and production were still evident during the snowmelt freshet and following precipitation events after 3 years. Effects of the burn were strongly influenced by the regional flow regime, with the most elevated N concentrations and production occurring during higher discharge periods (snowmelt freshet and storm flows).
引用
收藏
页码:2359 / 2371
页数:13
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