mark campbell. brief intro of wetlands turkey creek wetland a restored floodplain wetland at a...
Post on 19-Dec-2015
217 views
TRANSCRIPT
Constructed Wetlands and the soil properties and biogeochemical processes
that increase efficiency in Nitrate removal
Mark Campbell
Brief Intro of Wetlands
Turkey Creek WetlandA restored floodplain wetland at a private farm in rural McLean
County, Illinois
Characteristics of Wetlands
Wetlands are transitional areas between land and water
Main Characteristic present of surface or near-surface water, at least periodically
The hydrology of wetlands is generally one of slow flows and either shallow waters or saturated substrates
Also forms an Anaerobic environment
Benefits CostsProvides the removal of
contaminants: Nitrates, Phosphorous, metalloids
Allows for sedimentation to occur
Low Cost Removal as opposed to Ion-Exchange
Control of FloodingEcosystem for wildlife
Loss of Land use $$$$
Aesthetic Value
Differences between Soils in Constructed and Natural Wetlands
5 cm Depth20 cm Depth
Variable CW Reference
Organic (%)
4.8 11.5
Sand Content (%)
52.1 23.7
Clay (%) 22.0 30.0
Silt (%) 20.0 45.2
CW Reference
2.8 7.2
54.3 21.9
30.1 31.4
15.0 39.5
Campbell et al (2002)
ComparisonIt was also found that the diversity of plant
communities were higher in reference sites
Even in long-term CW’s the organic matter did not reach levels of reference sitesThis has shown to be an indicator of removal of
nitrogen (Reddy and D’Angelo 1997).
Factors that affect Denitrification rates
Temperature With season, can not control, lower temp. lower
rate
pH pH in natural waters is in the between 6 to 8,
optimal pH for denitrifying bacteria
Redox Potential Organic Carbon and Dissolved Oxygen
Retention time/Flow Rate
Biochemistry Organic Material is oxidized by aerobic
respiration use Oxygen as the electron receptor, while anaerobic conditions use Nitrogen as receptor (Metcalf and Eddy 2003).
Corganic + 4 NO3- + 4H+ = 2N2 + 5CO2
+ 2H2O
PseudomonasThiobacillus
Constructed wetlands have found to remove ≈40% of NO3- ther is
a high degree of variability there have been reports of up to 75% and low of 15% (Kovacic et al. 2000)
Flow Rate and Retention TimeDuring pulse flows, in the case of storm
events the amount of denitrification is greatly reduced (Kovaic 2006).
Still wetlands need slow flow, to have some mixing in the water. Need to create anaerobic environment.
The average retention time 6-8 days for optimal conditions (Zedler 2003).
Horizontal substrate is more important, while increase in depth lowers efficiency(Garcia et al 2010).