The first site we visited was Cors Erddreiniog which we previously visited during the LIFE conference a blog on which can be found here.
This time however we had to get our hands dirty! We started the day with some talks, then split into groups to measure diversity using quadrats, plunge sticks to measure peat depth and measuring pH and conductivity of the soil with special appliances.
The Migneint is the second site we visited, it is the largest area of blanket bog in the UK and is situated in central Snowdonia. It is a Special Area of Conservation (SAC) and work has been carried out to help restore it since large areas have been damaged by ongoing afforestaion, drainage, grazing and also burning, in hopes to make it better for agriculture. Being an important breeding ground for Hen Harriers it is in the interest of many to bring the area back to its full potential including the RSPCA who have been undertaking many projects which can be found here. An interesting article and video can be found on the BBC website giving an insight into the conservation efforts of the site.
At the Migneint there were strange peat erosion complexes, these are where the peat has been degraded possibly due to the previous drainage issues at the site meaning the peat gets an influx of oxygen which increases degradation. These complexes show how deep the peat could have been if the site was left in its natural state.
Differences
The main visual difference when comparing the two sites is definitely the height of the vegetation.Walking along the boardwalks at Cors Erddreiniog you are surrounded by vegetation almost at eye level, whereas at the Migneint the vegetation is almost all low lying comprising mainly of mosses and Juncus. The main reasoning for this could be that the water supply for blanket bogs is nutrient poor as it all comes from precipitation in comparison to the Cors Erddreiniog fen which is fed by a mixture of rain water and groundwater increasing nutrient levels and improving primary production. Conductivity was much higher at the fen and pH was recorded to be close to neutral, due to the calcium ions increasing the pH compared to the lower pH of the Migneint and also the lower conductivity.


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