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Fen Management Handbook - Scottish Natural Heritage

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Surface water level change e.g.<br />

– a climatic drier or wetter period (e.g. a few years) that is expected to occur<br />

naturally every so often;<br />

– past and recent management or dereliction of water course;<br />

– recent management (or dereliction) of culverts / sluices / outflow valves;<br />

– recent flood management in the catchment (river / lake levels are now different);<br />

– new or changed flood embankment;<br />

– changed variability (frequency and intensity of rainfall events) due to long-term<br />

climate change.<br />

Groundwater level change<br />

– a climatic drier or wetter period (e.g. a few years) that might be expected to<br />

occur naturally every so often;<br />

– changes in groundwater abstraction quantity or location;<br />

– reduced recharge due to long term climate change and land management<br />

changes within the recharge area.<br />

7.1.5 Consider what can be done about the changes<br />

Solutions to redress factors which have negatively influenced hydrology are<br />

summarised below. Practical aspects of lowering ground level and raising water<br />

tables are described in more detail in the text which follows.<br />

Remedy/options Considerations<br />

Problem: Ground water drying up<br />

Remedy: Increase soligenous supply<br />

Raise the water level in the aquifer by increasing<br />

catchment recharge through appropriate land<br />

management.<br />

Decrease abstraction from the aquifer at specific times<br />

and by amounts that will have a beneficial impact on<br />

discharge to the fen.<br />

Artificially increase groundwater level. If possible, and if<br />

reduced groundwater supply is due to a local de-watering<br />

for example, a re-charge trench can be installed between<br />

the fen and the abstraction to raise the groundwater level.<br />

Problem: Surface water, fen too dry<br />

Remedy: Increase topogenous supply<br />

(a) Increase water retention on the fen by restricting<br />

outflow (blocking ditches / changing levels of weirs).<br />

Requires discussions with environmental regulators and<br />

external specialist support.<br />

Normally only realistic where the fen is legally protected<br />

(e.g. SSSI / ASSI or Natura 2000), will require specific<br />

investigations and could be very costly. This will require<br />

discussions with environmental regulators and external<br />

specialist support<br />

Temporary solution and costly in terms of both finance<br />

and energy, but might be the only solution in certain<br />

cases. This will require discussions with environmental<br />

regulators and external specialist support<br />

Standing water may result in anoxia especially in peat or<br />

soils rich in organic matter. Care should be taken that<br />

no standing water remains continually on the surface,<br />

or the fen may change to a swamp which will be harder<br />

to manage. In ‘flow through fens’ such as alkaline fens,<br />

water should be kept moving through the soil. This kind<br />

of management might need consent from environmental<br />

regulators and can affect adjoining landowners.<br />

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