Impact of Precipitation Intensity and Riparian Geomorphic Characteristics on Greenhouse Gas Emissions at the Soil-Atmosphere Interface in a Water-Limited Riparian Zone

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• 作者：P. Vidon ; S. Marchese ; M. Welsh ; S. McMillan
• 关键词：Riparian zones ; Greenhouse gases ; Water limitation ; Precipitation ; Geomorphology
• 刊名：Water, Air, and Soil Pollution
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：227
• 期：1
• 全文大小：1,468 KB
• 参考文献：Atkin, O. K., Edwards, E. J., & Loveys, B. R. (2000). Response of root respiration to changes in temperature and its relevance to global warming. New Phytologist, 147(1), 141鈥?54.CrossRef
  Bowden, R. D., Castro, M. S., Melillo, J. M., Steudler, P. A., & Aber, J. D. (1993). Fluxes of greenhouse gases between soils and the atmosphere in a temperate forest following a simulated hurricane blowdown. Biogeochemistry, 21(2), 61鈥?1.CrossRef
  Burford, J. R., & Bremner, J. M. (1975). Relationships between the denitrification capacities of soils and total water-soluble and readily decomposable soil organic matter. Soil Biology and Biochemistry, 7, 389鈥?94.CrossRef
  Clement, J. C., Pinay, G., & Marmonier, P. (2002). Seasonal Dynamics of denitrification along topohydrosequences in three different riparian wetlands. Journal of Environmental Quality, 31, 1025鈥?037.CrossRef
  Clesceri, L. S., Greenberg, A. E., & Eaton, A. D. (1998). Standard methods for the examination of water and waste water. Washington, D.C.: American Public Health Association.
  Devito, K. J., Fitzgerald, D., Hill, A. R., & Aravena, R. (2000). Nitrate dynamics in relation to lithology and hydrologic flow path in a river riparian zone. Journal of Environmental Quality, 29, 1075鈥?084.CrossRef
  Fisher, K., Jacinthe, P. A., Vidon, P., Liu, X., & Baker, M. E. (2014). Nitrous oxide emission from cropland and adjacent riparian buffers in contrasting hydrogeomorphic settings. Journal of Environmental Quality, 43(1), 338鈥?48. doi:10.鈥?134/鈥媕eq2013.鈥?6.鈥?223 .CrossRef
  Groffman, P. M., Butterbach-Bahl, K., Fulweiler, W., Gold, A., Morse, J., Stander, E., Tague, C., Tonitto, C., & Vidon, P. (2009). Incorporating spatially and temporally explicit phenomena (hotspots and hot moments) in denitrification models. Biogeochemistry, 93, 49鈥?7. doi:10.鈥?007/鈥媠10533-008-9277-5 .CrossRef
  Harms, T. K., & Grimm, N. B. (2012). Responses of trace gases to hydrologic pulses in desert floodplains. Journal of Geophysical Research, Biogeosciences, 117, G01035. doi:10.鈥?029/鈥?011JG001775 .
  Harrison, M.D., Miller, A.J., Groffman, P.M., Mayer, P.M., & Sujay, S.K. (2014) Hydrologic controls on nitrogen and phosphorous dynamics in relict oxbow wetlands adjacent to an urban restored stream. Journal of the American Water Resources Association, 1鈥?8, doi:10.1111/jawr.12193
  Hedin, L. O., von Fischer, J. C., Ostrom, N. E., Kennedy, B. P., Brown, M. G., & Robertson, G. P. (1998). Thermodynamic constraints on nitrogen transformations and other biogeochemical processes at soil-stream interfaces. Ecology, 79, 684鈥?03.
  Jacinthe, P. A., Vidon, P., Fisher, K., Liu, X., & Baker, M. E. (2015). Methane and carbon dioxide fluxes in adjacent cropland and riparian buffers. Journal of Environmental Quality. doi:10.鈥?134/鈥媕eq2015.鈥?1.鈥?014 .
  Jacinthe, P. A., & Dick, W. A. (1997). Soil management and nitrous oxide emissions from cultivated fields in southern Ohio. Soil & Tillage Research, 41(3鈥?), 221鈥?35.CrossRef
  Jacinthe, P. A., Groffman, P. M., Gold, A. J., & Mosier, A. (1998). Patchiness in microbial nitrogen transformations in groundwater in a riparian forest. Journal of Environmental Quality, 27, 156鈥?64.CrossRef
  Jacinthe, P. A., & Lal, R. (2004). Effects of soil cover and land-use on the relations flux-concentration of trace gases. Soil Science, 169(4), 243鈥?59.CrossRef
  Jacinthe, P. A., Bills, J. S., Tedesco, L. P., & Barr, R. C. (2012). Nitrous oxide emission from riparian buffers in relation to vegetation and flood frequency. Journal of Environmental Quality, 41(1), 95鈥?05. doi:10.鈥?134/鈥媕eq2011.鈥?308 .CrossRef
  IPCC. 2013. Climate Change 2013: The Physical Science Basis: Working Group I Contribution to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Stocker TF, Qin D, Plattner GK, Tignor M, Allen SK, Boschung J, Nauels A, Xia Y, Bex V, Midgley PM (eds.) Cambridge, UK: Cambridge University Press
  Karl, T. R., & Knight, R. W. (1998). Secular trends of precipitation amount, frequency, and intensity in the United States. Bulletin of the American Meteorological Society, 79, 231鈥?41.CrossRef
  Milly, P. C. D., Dunne, K. A., & Vecchia, A. V. (2005). Global pattern of trends in streamflow and water availability in a changing climate. Nature, 438, 347鈥?50.CrossRef
  Mitsch, W.J., & Gosselink, J.G. (2000) Wetlands. New York: Wiley, p. 920.
  Morse, J. L., Ard贸n, M., & Bernhardt, E. S. (2012). Greenhouse gas fluxes in southeastern US coastal plain wetlands under contrasting land uses. Ecological Applications, 22(1), 264鈥?80.CrossRef
  Naiman, R. J., Decamps, H., & McClain, M. E. (2005). Riparia: ecology, conservation, and management of streamside communities. London, UK: Elsevier Academic Press. 430 pp.
  Nelson, D. W., & Sommers, L. E. (1996). Total carbon, organic carbon, and organic matter. In D. L. Sparks (Ed.), Methods of soil analysis, part 3鈥撯€揷hemical methods (pp. 961鈥?010). Madison, WI: Soil Science Society of America.
  Riveros-Iregui, D. A., & McGlynn, B. L. (2009). Landscape structure control on soil CO2 efflux variability in complex terrain: scaling from point observations to watershed scale fluxes. Journal of Geophysical Research, Biogeosciences, 114(G2), G02010.
  Rook, S.P. (2012) Riparian zone hydrology and biogeochemistry as a function of stream evolution stage in a glaciated landscape of the U.S. Northeast. MS Thesis, SUNY-ESF, 102 p. http://鈥媑radworks.鈥媢mi.鈥媍om/鈥?5/鈥?4/鈥?514403.鈥媓tml
  Tuttle, A. K., McMillan, S. K., Gardner, A., & Jennings, G. D. (2014). Channel complexity and nitrate concentrations drive denitrification rates in urban restored and unrestored streams. Ecological Engineering, 73, 770鈥?77. doi:10.鈥?016/鈥媕.鈥媏coleng.鈥?014.鈥?9.鈥?66 .CrossRef
  Ullah, S., & Moore, T. R. (2011). Biogeochemical controls on methane, nitrous oxide, and carbon dioxide fluxes from deciduous forest soils in eastern Canada. Journal of Geophysical Research, Biogeosciences, 2005鈥?012, 116 (G3).
  Vidon, P., & Hill, A. R. (2004). Denitrification and patterns of electron donors and acceptors in eight riparian zones with contrasting hydrogeology. Biogeochemistry, 71(2), 259鈥?83.CrossRef
  Vidon, P., Allan, C., Burns, D., Duval, T. P., Gurwick, N., Inamdar, S., Lowrance, R., Okay, J., Scott, D., & Sebestyen, S. (2010). Hot spots and hot moments in riparian zones: potential for improved water quality management. Journal of the American Water Resources Association, 46(2), 278鈥?98.CrossRef
  Vidon, P., Jacinthe, P. A., Liu, X., Fisher, K., & Baker, M. (2014). Hydrobiogeochemical controls on riparian nutrient and greenhouse gas dynamics: 10 years post-restoration. Journal of the American Water Resources Association, 50(3), 639鈥?52. doi:10.鈥?111/鈥媕awr.鈥?2201 .CrossRef
  
• 作者单位：P. Vidon (1)
  S. Marchese (1)
  M. Welsh (1)
  S. McMillan (2)
  
  1. College of Environmental Science and Forestry (SUNY-ESF), The State University of New York, 320 Bray Hall, 1 Forestry Drive, Syracuse, NY, 13210, USA
  2. Purdue University, 225 South University Street, West Lafayette, IN, 47907, USA
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Environment
  Environment
  Atmospheric Protection, Air Quality Control and Air Pollution
  Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
  Terrestrial Pollution
  Hydrogeology
  
• 出版者：Springer Netherlands
• ISSN：1573-2932

文摘

As concentrations of greenhouse gases (GHG: N₂O, CO₂, CH₄) continue to increase in the earth鈥檚 atmosphere, there is a need to further quantify the contribution of natural systems to atmospheric GHG concentrations. Within this context, characterizing GHG contributions of riparian zones following storms events is especially important. This study documents soil GHG effluxes in a North Carolina riparian zone in the days following both a natural 2.5-cm precipitation event, and that same event associated with the addition of 8.7 cm artificial rainwater in select static chambers. No significant differences in CO₂, CH₄, and N₂O fluxes in response to increased moisture were observed between a depression, a sand bar, and an upland forested area. However, in this water-limited riparian zone, less negative CH₄ fluxes (i.e., methane oxidation decreased) and higher CO₂ fluxes (i.e., aerobic respiration increased) were observed following precipitation. A short-term burst in N₂O emission was observed in the hours after precipitation occurred, but elevated N₂O emissions did not persist long enough to turn the site from the N₂O sink to a N₂O source in the 3 days following the beginning of the experiment. Our results are in contrast with riparian GHG studies in wetter environments and illustrate the importance of water limitation in regulating riparian soil response to precipitation with respect to GHG emissions. More studies should be conducted in water-limited environments (e.g., US southeast/southwest) before management strategies commonly applied in wetter environments (e.g., US Northeast/Midwest) are applied in these regions. Keywords Riparian zones Greenhouse gases Water limitation Precipitation Geomorphology