Hill,A.R.(2011): Buried organic-rich horizons: their role as nitrogen sources in stream riparian zones. Biogeochemistry, 104, 347-363.

『埋没した有機に富む層:河岸帯における窒素源としてのそれらの役割』


Abstract
 The effect of water table fluctuations on the interaction between nitrogen mineralization in buried organic-rich soil horizons and nitrate mobilization into groundwater was examined in the riparian zone of a small headwater agricultural catchment in southern Ontario, Canada. Riparian soils contained buried organic layers and lenses overlying a poorly sorted gravel layer at a depth of 0.8-1.0 m. The riparian water table in summer 2006 generally remained within 0.4 m of the surface, whereas during a major drought in 2007 the water table declined to >1.9 m in August and riparian soils above the gravel layer inland from the stream remained unsaturated from mid-June to early November. mean daily net N mineralization and nitrification rates during 2-4 week in situ soil incubations were 0.2-1.35 mg N kg-1 day-1 in 0-10 cm surface soils in May-September 2006, whereas N mineralization and nitrification were negligible at 30-45 and 60-75 cm soil depths. In summer and fall 2007, high daily rates of n mineralization and nitrification of 0.3-0.8 mg N kg-1 day-1 occurred at 30-45 and 60-75 cm depths that were similar to surface soil rates. The soil nitrate pool at 60-75 cm depth was 16× larger in autumn 2007 in comparison to 2006. During high water tables in November 2006 groundwater in the gravel layer had low NO3-N concentrations of <0.1 mg l-1. In contrast, after the drought in 2007 nitrate was flushed into groundwater as the water table rose to within 30-50 cm of the surface in December. An extensive area of high NO3-N concentrations (3-18 mg l-1) occurred inland from the stream bank. This zone of high nitrates declined gradually by April 2008 probably as a result of denitrification. These results indicate that buried organic deposits at depth within riparian areas can be important nitrogen sources during major water table drawdowns. The influence of these episodes of mineralization at depth during droughts on riparian groundwater chemistry and the emissions of greenhouse gases to the atmosphere merit further research.

Keywords: Riparian zone; Net N mineralization; Nitrification; Water table; Soil organic matter; Groundwater』

Introduction
Study sites
Methods
 Soil sampling
 Nitrogen mineralization and nitrification
 Groundwater hydrology and chemistry
Results
Soil organic carbon and nitrogen contents
 Water table fluctuations and groundwater flow patterns
 Net nitrogen mineralization and nitrification
 Ammonium and nitrate pools
 Groundwater nitrogen
Discussion
 Buried stores of organic matter
 Impact of water table fluctuations on soil n dynamics
 Nitrate mobilization into riparian groundwater
 Export of mobilized groundwater nitrate to streams
 Riparian zone characteristics in relation to subsurface N mineralization and nitrate mobilization
Conclusion
Acknowledgements
References


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