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Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
Clad agm forest research_nadeem
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Clad agm forest research_nadeem

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  • 1. Flanders Moss: The Effects of BogRestoration on Drainage Water Chemistry Nadeem Shah Forest Hydrology Centre for Forestry and Climate Change
  • 2. Rationale Peatland Conservation • The importance of peatland conservation and restoration is now well recognised. • However the impact of restoration on soil and water has not been fully investigated. • What are the effects of peatland restoration on drainage water chemistry? • What are the effects on freshwater ecology? • What can be done to prevent or minimise impacts?2 09/03/2011
  • 3. Freshwater Ecology Freshwater Pearl Mussel • Found only in clean rivers and streams; now threatened with extinction throughout its holarctic range. • In Scotland viable populations still remain and are the focus of conservation action. • Environmental factors? Most likely causes • oxygen deficiency caused by chronic eutrophication - Nutrient and sediment pollution from agriculture - Clearfelling in the uplands - Sewage discharges - Aquaculture discharges3 09/03/2011
  • 4. Phosphate risk? • In Ireland there was a series of significant FWPM kills. • The main cause was considered to be raised phosphate levels within run-off from peatland forestry following clearfelling (algal blooms) which led to a moratorium on clearfelling in catchments identified as sensitive for FWPM. • Cummins and Farrell (2003) found that phosphate concentrations increased following clearfelling on peatlands. • Most other studies assessing the impact of clearfelling on drainage water have provided little evidence of raised phosphate levels after felling. • However these studies have been on mineral soils which have a higher phosphate sorption capacity than peat.4 09/03/2011
  • 5. Carbon Increased DOC in surface waters • atmospheric CO2 concentration • climate warming • continued N deposition • decreased sulfate deposition (DOC more soluble as acidity and ionic strength increase.) • hydrological changes due to increased precipitation, droughts, and land use change • Another FR study at Flanders Moss looking at effects of restoration on greenhouse gas flux.5 09/03/2011
  • 6. Aims Flanders Moss • Investigate the effects of bog restoration, through clearfelling, on drainage water chemistry. • Quantify changes in nutrients (particularly phosphate) and DOC following restoration. • Recommendations to improve best practice. • Guidance for restoration.6 09/03/2011
  • 7. Location Figure 1 Flanders Moss location7 09/03/2011
  • 8. Background Background • Flanders Moss - raised bog and part of Achray Forest on the floodplain of the River Forth. • Organic rich peaty gley soil -Sphagnum/Eriophorum peat up to 8.5 m deep (average 4.6 m). • The land has been drained since the 1920’s, initially to improve grouse shooting. • Drained and ploughed in 1964/65 for a silvicultural experiment. • Planted with Lodgepole Pine and Sitka Spruce; phosphate fertilizer application around each tree in 19658 09/03/2011
  • 9. Experimental Set-up• Three sampling points; one control catchment.• Two drains and a natural stream (Blackrat burn)• Fortnightly water sampling began in 2008• Major inorganic anions and cations DOC, conductivity, pH, colour, suspended solids and occasional ICP. Figure 2 Aerial photograph of Flanders Moss showing sampling points.9 09/03/2011
  • 10. Water level recorder • Installed automatic pressure and temperature sensor - depth and temperature reading every 15 minutes. • Rating the channels • Convert chemical concentrations to fluxes. Figure 3 Water level recorder and stilling well at Flanders Moss Site 310 09/03/2011
  • 11. Data collection • Clearfelling delayed due to on-site problems • One area was clearfelled in winter 09/10 • Preliminary data11 09/03/2011
  • 12. Preliminary results Figure 4 P(PO4) and N(NO3) in Flanders Moss drainage water; vertical lines indicate clearfelling period at Site 1 • Phosphate concentration increases following felling • Delayed response – (brash dries out and phosphate is leached.) • Is there more P to come? Will regrowth of vegetation prevent further leaching– recycling of P12 09/03/2011
  • 13. Preliminary Results Figure 5 Colour and DOC in Flanders Moss drainage water; vertical lines indicate clearfelling period at Site 1 • Colour and DOC increase following felling period • Is there more DOC to come in Spring/Summer 2010?13 09/03/2011
  • 14. Preliminary Results Figure 6 pH and suspended solids in Flanders Moss drainage water; vertical lines indicate clearfelling period at Site 1 • pH increase at Site 1 following felling – proximity to road?14 09/03/2011
  • 15. Notes Points to note • Clearfelling led to an increase in Phosphate and DOC in drainage waters. • Too early to draw any conclusions on the environmental impacts. • Monitoring of clearfelled site is ongoing and further clearfelling is planned. • Implications for management and restoration - depending on proportion of catchment felled, catchment size, receiving waters and local ecology15 09/03/2011
  • 16. Thank you Thank you16 09/03/2011

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