Topsoil.
The majority of mineral nutrients and organic material is found in the topsoil layer of soil. Topsoil is typically rich in nutrients and organic matter due to the presence of decomposing plant and animal material, as well as microbial activity that helps break down organic matter into nutrients.
Organic Layer - plant litter Surface Layer - mineral and organic mixture Subsoil - contains clay, iron, aluminium Substratum - parent material
O-Horizon: leaf litter, organic material A-Horizon: plough zone, rich in organic matter B-Horizon: zone of clay, iron and organic matter C-Horizon: weathering zone, little organic matter and little life R-Horizon:unweathered parent materia
The layer that contains the most organic material in the diagram is the top layer, known as the O horizon or organic horizon. This layer is made up of decomposing organic matter such as leaf litter and other plant debris.
Yes, soil is composed of weathered rocks, minerals, decomposed organic material (humus), water, and air. This mixture forms the top layer of the Earth's surface and provides a medium for plant growth.
Topsoil is the uppermost layer of soil that contains organic matter and is crucial for plant growth. Subsoil is the layer beneath topsoil that is lower in organic matter and contains more minerals. Bedrock is the solid rock layer beneath subsoil that serves as the parent material for soil formation.
It is the O horizon. The A horizon is the mineral horizon and does include a large amount of organic material but the O horizon contains the most abundant amount of organic matter. The O horizon overlies the A horizon.
The organic level which is the uppermost level of the soil.
Soil typically has distinct layers, or horizons, that are created by the weathering of rock and the accumulation of organic matter. The top layer, known as the O horizon, is rich in organic material. Below that is the A horizon, or topsoil, which contains a mix of organic material and minerals. The B horizon, or subsoil, is characterized by the accumulation of minerals leached from the upper layers. Finally, the C horizon consists of partially weathered rock material.
The O horizon is the top layer made of organic material like plant litter. The A horizon is rich in organic matter and minerals, where most root activity occurs. The B horizon is known as the subsoil, containing minerals leached from the upper layers.
The top of the soil profile consists of the O horizon (organic layer) followed by the A horizon (topsoil). The O horizon contains organic matter like leaf litter and decomposing plant material, while the A horizon is rich in minerals, nutrients, and organic material which supports plant growth.
the crust