talajrétegzdés
Talajrétegződés, also known as soil stratification or soil horizons, refers to the distinct layers that develop in a soil profile over time. These layers, or horizons, are created by various soil-forming processes acting on the parent material. The most common horizons, starting from the surface and going downwards, are typically denoted as O, A, E, B, and C.
The O horizon is the uppermost layer and consists primarily of organic matter, such as decomposing leaves,
The E horizon, if present, is a leached layer beneath the A horizon. Here, minerals like iron
Finally, the C horizon consists of partially weathered parent material, with little organic matter present. Below