sort of well, only 18% the other things that make up horizon B is oxygen, vitamins, and cows
The B horizon develops as rainwater washes clay and minerals from the A horizon to the B horizon below it. This process is called leaching. The B horizon typically contains more clay and accumulated minerals than the A horizon.
The B horizon typically contains minerals, organic matter, and clay particles that have been leached down from the A horizon above. It is often characterized by an accumulation of minerals like iron, aluminum, and clay.
The C horizon contains mainly parent material, while the B horizon contains mainly clay particles and the A horizon; mainly silt sized particles and humus
The B horizon is rich in minerals leached from the A horizon above and can exhibit a higher clay content. The A horizon is the topmost layer commonly consisting of organic matter mixed with mineral particles. The C horizon is a layer of weathered and broken rock material beneath the B horizon.
The B horizon typically contains clay, organic matter, minerals, and nutrients that have leached down from the topsoil and accumulated. It is often richer in nutrients than the underlying C horizon.
The B horizon is also called the subsoil. It is a soil layer that is located beneath the topsoil layer (A horizon) and typically contains less organic matter and more clay, iron, and minerals.
The B horizon is known as the zone of accumulation because it is where minerals and nutrients that have leached from the A horizon above accumulate. These substances, like clay, iron, and organic matter, accumulate in the B horizon due to the downward movement of water through the soil profile.
The B horizon in soil profiles often has a higher accumulation of clay, iron, or organic matter compared to the A horizon. It can also show evidence of leaching with the movement of minerals and nutrients downslope. The B horizon typically has a darker color and a structure that is more dense and compact compared to the overlying A horizon.
Because the A horizon contains more humus which makes the A horizon more organic
There are many things that horizon A and horizon B could form. These things include slopes and lines for example.
A horizon is often darker than B horizon or C horizon because it is the topsoil and the topsoil might be covered with litter. The litter decompose and as you know become soil and it will be fresh soil. So the fresh soil is darker than B and C horizon
The second layer of a soil profile is called the B horizon. It is located beneath the topsoil (A horizon) and is often characterized by an accumulation of minerals leached from the topsoil above. The B horizon typically has a higher clay content and can also contain iron or aluminum oxides.