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Fen Management Handbook - Scottish Natural Heritage

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<strong>Management</strong> objectives for a wetland site can rarely be set in isolation from the<br />

surrounding land. It is possible, for example, that wetting up a fen may cause<br />

wetting up in adjacent non-fen land, especially if this land was originally part of<br />

the same wetland. The consequences of proposed management, particularly<br />

installation or removal of structures which may influence water level, should be<br />

carefully considered and neighbouring land owners/managers consulted at the<br />

earliest opportunity. See Section 11: <strong>Fen</strong>s and People.<br />

5.8.5 Defining a target hydrological regime<br />

Defining an ideal or target hydrological regime for a particular fen can be<br />

considered at various levels depending on available resources, level of<br />

understanding or available information and the level of detail required.<br />

– At the most basic level, for example for fen management undertaken through<br />

agri-environment schemes, defining a target hydrological regime involves<br />

determining which areas of a site (linked to the ecology) should be ‘wet’ i.e.<br />

with soil water levels within 10 cm of the ground surface during the summer<br />

months, and which should not fall more than 30 cm below ground surface for<br />

any significant period of time (say one month). This could be based upon local<br />

knowledge or on published guidance, such as the eco-hydrological guidelines<br />

described below.<br />

– At a more complex level, it may be necessary to identify the key water transfer<br />

mechanisms for the site and some simple spatial (i.e. site or location specific)<br />

and/or temporal (seasonal or time specific) criteria for the operation of these.<br />

For example, perennial flow might be required from a set of springs within a<br />

sloping fen, or complete inundation by overbank flooding might be required<br />

annually for a tall-herb fen on a floodplain.<br />

– At the highest level, for example more ambitious fen management schemes or<br />

those which might affect a public water supply, a lot more detail will be required,<br />

but identification of the precise hydrological requirements of many species and<br />

habitats is limited by lack of research or confinement of current research to a<br />

limited geographical area.<br />

Historically, most wetland management was decided on the basis of expert<br />

judgement or reactive management. Recently, driven primarily by the obligation<br />

to conserve wetlands in a number of European Community Directives (such as<br />

92/43/EEC: Conservation of <strong>Natural</strong> Habitats and of Wild Fauna and Flora),<br />

ecohydrological guidelines have been developed for lowland wetland plant<br />

communities (Wheeler et al, 2004), including wet grassland, fen and mire, ditch<br />

and swamp communities, and wet woodlands (Barsoum et al, 2005), covering the<br />

different types of wet woodland habitat.<br />

Ecohydrological guidelines are based on the NVC system for plant communities<br />

(see Appendix IV). For example, for S24 (Phragmites australis–Peucedanum<br />

palustre) tall-herb fen, Wheeler et al (2004) include:<br />

90<br />

Optimal water levels. Summer water level is typically around 15 cm below<br />

ground level, but deeper levels may be a perfectly natural feature of some sites.<br />

The sub-community most often associated with a water level at or near the<br />

surface all year round (S24e) on average supports the greatest number of rare<br />

species. Winter inundation is a natural feature of many S24 stands.<br />

Sub-optimal or damaging water levels. Strongly sub-surface winter and<br />

summer water tables are outside the normal range of this community; peat<br />

drying and degradation would lead to development of rank fen rapidly becoming<br />

wooded without management. Very wet sites with widespread summer

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