A. The A horizon.
Horizon B may contain minerals from Horizon A due to processes such as leaching, where minerals are moved downwards by water percolating through the soil. As the water moves through the soil profile, it can dissolve minerals from Horizon A and transport them to Horizon B. This process of mineral movement is known as translocation.
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
Eluviation is the process of removing fine mineral particles from a horizon, while illuviation is the deposition of these particles in a different horizon. As material is leached from one horizon (B horizon) due to water percolation, it gets deposited in a lower horizon (B horizon) where it accumulates. This leads to the formation of distinct soil horizons with varying characteristics based on the movement and accumulation of materials.
The soil horizon that is made up of partially broken bedrock is known as the C horizon. It is located directly beneath the B horizon and consists of weathered rock fragments intermingled with some organic material.
C-Horizon is a layer in the soil profile that consists of weathered parent material. It is located beneath the B-Horizon and contains partially weathered rock fragments. The C-Horizon is important for providing nutrients to plants as it undergoes further weathering and contributes to soil formation over time.
Horizon B's name is Horizon Brave.
A & B Horizon forms wherever bedrock is exposed.
A & B Horizon forms wherever bedrock is exposed.
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.
There are many things that horizon A and horizon B could form. These things include slopes and lines for example.
There are many things that horizon A and horizon B could form. These things include slopes and lines for example.
horizon A , horizon B and horizon C
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.
b horizon
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
Materials that leach from horizon A are typically deposited into horizon B, also known as the subsoil. This horizon can accumulate minerals, clays, and organic matter that have been leached from the upper layers.
The B horizon is the layer of soil underneath the A horizon, which is under the O horizon. The B horizon contains minerals and sand grains as well as organic material. If you didn't get it when your teacher explained it, ask him/her aboput it. They are sure to explain better than I can!