zandgronden
Zandgronden are soils that consist mainly of sand and are characterized by a light, gritty texture, rapid drainage and a relatively low capacity to hold nutrients and water. Their high porosity allows quick water movement through the profile, which often results in drought stress in dry periods and frequent leaching of minerals, especially in exposed locations. The organic matter content is typically low, and pH tends to be more acidic unless limed.
Zandgronden originate from wind-blown sands or glacial outwash sands and are common in regions with historic
Soil properties and implications
The sandy texture gives high aeration and drainage, but limits water storage and nutrient retention. The low
Zandgronden are used for arable farming and grassland where they are adequately managed. Typical agricultural practices
Natural vegetation on zandgronden includes heaths and sandy grassland communities. Protection against erosion and nutrient leaching