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Fen Management Handbook - Scottish Natural Heritage

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4. Understanding <strong>Fen</strong> Nutrients<br />

Nutrient levels have a significant effect on fen vegetation,<br />

biodiversity and nature conservation value. Understanding<br />

how and why nutrient regimes are subject to change, and the<br />

problems which can arise as a result, is therefore critical to fen<br />

management.<br />

This section explains the basic principles of nutrient enrichment in<br />

relation to fens and considers key factors which affect fen nutrient<br />

regimes. It also outlines methods of identifying and monitoring<br />

nutrient enrichment. Guidance on nutrient management is<br />

summarised in Section 8: Managing <strong>Fen</strong> Nutrient Enrichment.<br />

Key terminology used in relation to nutrients – glossary:<br />

Nutrients The chemical building blocks of plants, the most significant of which are the macronutrients N<br />

(nitrogen), P (phosphorus) and K (potassium).<br />

Nutrient status<br />

Nutrient enrichment<br />

The amount of nutrients found in the fen.<br />

When there are more nutrients than might be considered desirable for particular fen habitats or<br />

features, also referred to as ‘eutrophication’. This is often caused by an increase in nutrient input<br />

over a short period of time into the system. ‘Cultural eutrophication’ is the term used to describe<br />

enrichment caused by human land management activities, typically intensive agriculture.<br />

Nutrient regime Describes the way nutrients enter, are used within, and leave a fen. As water is the key carrier for<br />

nutrients entering or leaving fens, the nutrient regime is closely linked to the hydrological regime,<br />

and is influenced by catchment geology, shape and land use, all of which affect the chemistry of<br />

water entering the fen.<br />

Nutrient availability The amount of nutrients available to plants is governed by a range of microbial and redox<br />

(reduction-oxidation) mediated processes in the soil. This means that the ‘plant-available’ pool of<br />

nutrients may be different to (often much smaller than) the total pool in the soil, which will include<br />

organically-bound forms less immediately available for plant uptake.<br />

Nutrient cycling <strong>Fen</strong> plants take up nutrients during their life, which are then (partly) released when the plant, or<br />

part of it, dies. The resulting nutrients are re-cycled by the soil microflora and re-used or re-cycled<br />

by other plants.<br />

Minerotrophic Wetlands receiving mineral inputs from groundwater, and/or surface runoff and/or over-bank<br />

flooding, as well as rainfall.<br />

Ombrotrophic Wetlands fed mainly by rainwater inputs (literally, fed by cloud inputs).<br />

Oligotrophic Soils and fen waters which are infertile – i.e. with small pools of available macronutrients.<br />

Mesotrophic<br />

Eutrophic<br />

Moderate fertility status.<br />

High fertility status. Some fens can be naturally high in nutrients, but often this term suggests<br />

some artificial enrichment.<br />

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