Sources and Transport of Nitrogen in Arid Urban Watersheds

被引:63
|
作者
Hale, Rebecca L. [1 ,4 ]
Turnbull, Laura [2 ,5 ]
Earl, Stevan [2 ]
Grimm, Nancy [1 ,2 ]
Riha, Krystin [6 ,8 ]
Michalski, Greg [7 ]
Lohse, Kathleen A. [9 ]
Childers, Daniel [3 ]
机构
[1] Arizona State Univ, Sch Life Sci, Tempe, AZ 85287 USA
[2] Arizona State Univ, Global Inst Sustainabil, Tempe, AZ 85287 USA
[3] Arizona State Univ, Sch Sustainabil, Tempe, AZ 85287 USA
[4] Univ Utah, Global Change & Sustainabil Ctr, Salt Lake City, UT 84112 USA
[5] Univ Durham, Dept Geog, Inst Hazard Risk & Resilience, Durham DH1, England
[6] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA
[7] Purdue Univ, Dept Chem, W Lafayette, IN 47907 USA
[8] Pacific NW Natl Lab, Richland, WA 99352 USA
[9] Idaho State Univ, Dept Biol Sci, Pocatello, ID 83209 USA
基金
美国国家科学基金会;
关键词
NITRATE SOURCES; SOLUTION CHEMISTRY; MISSISSIPPI RIVER; N-RETENTION; LAND USES; DENITRIFICATION; URBANIZATION; BIOGEOCHEMISTRY; DEPOSITION; ISOTOPES;
D O I
10.1021/es501039t
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Urban watersheds are often sources of nitrogen (N) to downstream systems, contributing to poor water quality. However, it is unknown which components (e.g., land cover and stormwater infrastructure type) of urban watersheds contribute to N export and which may be sites of retention. In this study we investigated which watershed characteristics control N sourcing, biogeochemical processing of nitrate (NO3-) during storms, and the amount of rainfall N that is retained within urban watersheds. We used triple isotopes of NO3- (delta N-15, delta O-18, and Delta O-17) to identify sources and transformations of NO3- during storms from 10 nested arid urban watersheds that varied in stormwater infrastructure type and drainage area. Stormwater infrastructure and land cover-retention basins, pipes, and grass cover-dictated the sourcing of NO3- in runoff. Urban watersheds were strong sinks or sources of N to stormwater depending on runoff, which in turn was inversely related to retention basin density and positively related to imperviousness and precipitation. Our results suggest that watershed characteristics control the sources and transport of inorganic N in urban stormwater but that retention of inorganic N at the time scale of individual runoff events is controlled by hydrologic, rather than biogeochemical, mechanisms.
引用
收藏
页码:6211 / 6219
页数:9
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