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Denitrification in an Urban Tidal Freshwater Wetland of the Delaware
T. Quirk, A. Smyth, M. Piehler, B. Horton, J. Mead, and D. J. Velinsky February 2010
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Tidal Freshwater Wetlands
Along coastal rivers Salinity less than 0.5 ppt Salt intolerant species Globally rare habitat Receive and process nutrient loads
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Organic N NO3- NH4+ flux N2 flux N2 (g) NO3+ flux NH4+
OO SEDIMENT WATER Organic N O NO3- Net Nitrification NH4+ flux N2 flux O N2 (g) Denitrification NO3+ flux Permanent removal O NH4+ Net Ammonification adapted from Kemp et al. 1990
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Denitrification varies temporally and spatially
Hypothesis Denitrification varies temporally and spatially Elevation Season Vegetation Soil and water N
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The Darby-Cobbs watershed
Cobbs Creek Darby Creek Stony Creek Muckinipattis Creek Hermesprota Creek
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Watershed Marsh Phragmites australis
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Low tide High tide
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Spatial variation - upstream, main marsh, downstream - low, mid-, high marsh plant communities / elevations
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Water Column Characteristics
b
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Seasonal aboveground biomass
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Denitrification Seasonal effect
B Seasonal effect Little spatial variation but a few hotspots of DNR No significant relationship between DNR and elevation or biomass
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APRIL Net flux of N from sediment to water column
OO SEDIMENT Organic N WATER O NO3- Net Nitrification NH4+ flux N2 flux O N2 (g) Denitrification NO3+ flux + 85 ± 27 µmol m-2 hr-1 + 474 ± 26 µmol m-2 hr-1 + 55 ± 29 µmol m-2 hr-1 O NH4+ Net Ammonification Net flux of N from sediment to water column Low rates of denitrification
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JULY Net flux of nitrate from water to sediment
OO SEDIMENT Organic N WATER O NO3- Net Nitrification NH4+ flux N2 flux O N2 (g) Denitrification NO3+ flux + 80 ± 21 µmol m-2 hr-1 - 293 ± 53 µmol m-2 hr-1 + 396 ± 43 µmol m-2 hr-1 O NH4+ Net Ammonification Net flux of nitrate from water to sediment High rates of denitrification
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OCTOBER Ammonium flux low and variable
OO SEDIMENT Organic N WATER O NO3- Net Nitrification NH4+ flux N2 flux O N2 (g) Denitrification NO3+ flux + 4 ± 9 µmol m-2 hr-1 - 327 ± 92 µmol m-2 hr-1 + 100 ± 9 µmol m-2 hr-1 O NH4+ Net Ammonification Ammonium flux low and variable Moderate rates of denitrification
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Positive relationship between NH4+ flux and N2 flux in July
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Sediment O2 Demand Increase in SOD - Reduces O2 availability - Limits nitrification Implications Both nitrification and water column NO3+ fueling DNR in July Water column NO3+ fueling DNR in Oct
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Conclusions Little spatial variation in DNR
Seasonal effects on plant community composition and % of biomass AND DNR April- many locations with no DNR July- greatest DNR with coupled nitrification-DNR + water column NO3+ fueling DNR October- lower DNR but water column NO3+ fueling DNR Calculation of % N load undergoing DNR limited by lack of adequate streamflow data
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