Full TGIF Record # 269641
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DOI:10.1007/s11252-016-0538-0
Web URL(s):https://link.springer.com/article/10.1007/s11252-016-0538-0/fulltext.html
    Last checked: 10/06/2017
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https://link.springer.com/content/pdf/10.1007%2Fs11252-016-0538-0.pdf
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Publication Type:
i
Refereed
Author(s):Hall, Steven J.; Baker, Michelle A.; Jones, Scott B.; Stark, John M.; Bowling, David R.
Author Affiliation:Hall and Bowling: Global Change and Sustainability; Bowling: Department of Biology, University of Utah, Salt Lake City; Baker and Stark: Department of Biology and the Ecology Center; Jones: Department of Plants, Soils, and Climate, Utah State University, Logan, UT; Hall: Department of Ecology, Evolution, and Organismal Biology, Iowa State University, Ames, IA
Title:Contrasting soil nitrogen dynamics across a montane meadow and urban lawn in a semi-arid watershed
Source:Urban Ecosystems. Vol. 19, No. 3, September 2016, p. 1083-1101.
Publishing Information:Andover, Hants, United Kingdom: Chapman and Hall
# of Pages:19
Related Web URL:https://link.springer.com/article/10.1007%2Fs11252-016-0538-0#Abs1
    Last checked: 10/06/2017
    Notes: Abstract only
Keywords:TIC Keywords: Comparisons; Fertilization program; Lawn maintenance; Pastures; Semiarid climates; Snow removal; Soil moisture; Chemical properties of soil; Nitrogen; Soil temperature; Urbanization; Watershed management
Abstract/Contents:"Urbanization substantially increases nitrogen (N) inputs and hydrologic losses relative to wildland ecosystems, although the fate of N additions to lawns and remnant grasslands remains contested. In montane semi-arid ecosystems, N cycling is often closely coupled to snowmelt (the dominant period of infiltration) and snow cover, which impact soil temperature and moisture. Here, we compared soil N dynamics between a fertilized and irrigated urban lawn and nearby riparian meadow in Salt Lake City, Utah during a snow manipulation experiment. Snow removal increased freeze/thaw events but did not affect N pools, microbial biomass, denitrification potential, or soil oxygen (O2). Mineral N was similar between sites despite lawn fertilization, but dissolved organic N (DON) was four-fold greater (2.1 ± 0.1 mg N l-1) in lawn soil water. Infiltration was lower in the lawn subsoil, and leaching losses (modeled with Hydrus) were small at both sites (< 2 kg N ha-1 y-1) despite substantial lawn fertilization. Lawn soil O2 fluctuated between 20.9 and 1.6 % following snowmelt and irrigation, but remained near 20 % in the meadow; the lawn had more reducing microsites as indicated by iron speciation. Post-snowmelt potential denitrification was six-fold greater in the lawn than the meadow. Lawns can potentially provide hotspots of denitrification in a semi-arid landscape that exceed some natural riparian ecosystems, whereas DON may represent an increasingly important form of N loss from lawns."
Language:English
References:52
Note:Tables
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Hall, S. J., M. A. Baker, S. B. Jones, J. M. Stark, and D. R. Bowling. 2016. Contrasting soil nitrogen dynamics across a montane meadow and urban lawn in a semi-arid watershed. Urban Ecosystems. 19(3):p. 1083-1101.
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DOI: 10.1007/s11252-016-0538-0
Web URL(s):
https://link.springer.com/article/10.1007/s11252-016-0538-0/fulltext.html
    Last checked: 10/06/2017
    Access conditions: Item is within a limited-access website
https://link.springer.com/content/pdf/10.1007%2Fs11252-016-0538-0.pdf
    Last checked: 10/06/2017
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
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