Koeien in weiland langs water

Peat as a source of greenhouse gases

During the reclamation of peatland the groundwater table is lowered. This causes the peat to settle, shrink and oxidize. As a result, the soil subsides. The largest land subsidence occurred in the 20th century due to efficient drainage, which was required to make peatlands suitable for agriculture and peat excavation. Peat soils are also threatened by wildfire.

During the decomposition and oxidation of peat, greenhouse gases are released (carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O)). Although water authorities in some regions are trying to prevent further lowering of the groundwater table, the processes of decomposition and land subsidence continue. The greenhouse gases contribute to the warming of the atmosphere. The land subsidence increases the risk of flooding and can cause damage to constructions, roads, cables and pipes. Water management becomes increasingly complex and expensive.

In order to reduce the emission of greenhouses gases and land subsidence in peatlands, we want to find out how these processes work. Wageningen University & Research examines these in field experiments and modelling studies.

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