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Format

JP2

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Publisher-reported update

2017-01-26

Wetlands mainly occur low in the landscape and form areas of groundwater discharge. This aids in the accumulation and composition of peat, as water moves slowly in wetlands. Local topography and sediment characteristics, such as an underlying low-permeability clay layer, can lead to wetlands acting as areas of recharge to groundwater and discharge to surface drainage. Water levels vary in wetlands due to climate, seasonal factors, and large water losses to evapotranspiration

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