A horizons are darker than B or C horizons because they contain more organic matter and are richer in nutrients. The organic matter in A horizons contributes to increased soil fertility, which supports higher plant growth. B and C horizons have less organic matter and are more mineral-rich, which makes them lighter in color.
Horizon A may contain darker soil due to a higher organic matter content from accumulated plant material or decomposition products. This organic matter can contribute to the soil's color, as well as its fertility and structure. Horizons B and C may have lower organic matter content, resulting in lighter soil color.
There are typically five soil horizons: O (organic), A (topsoil), E (eluviated), B (subsoil), and C (parent material). Each horizon has unique characteristics and plays a key role in soil composition and function.
The five soil horizons are O horizon (organic matter), A horizon (topsoil), E horizon (eluviated or leached layer), B horizon (subsoil), and C horizon (parent material). These horizons collectively make up the soil profile and influence soil characteristics and fertility.
The correct order of soil horizons, from top to bottom, is O horizon, A horizon, E horizon, B horizon, C horizon, and R horizon. It is important to note that not all soils have all these horizons, as they can vary depending on the specific conditions of the soil.
The three horizons of soil layers are the A horizon (topsoil), which is rich in organic matter and nutrients; the B horizon (subsoil), which contains minerals leached from the topsoil; and the C horizon (parent material), which is the weathered rock or sediment that the soil developed from.
Horizon A may contain darker soil due to a higher organic matter content from accumulated plant material or decomposition products. This organic matter can contribute to the soil's color, as well as its fertility and structure. Horizons B and C may have lower organic matter content, resulting in lighter soil color.
horizon A , horizon B and horizon C
O,A,B,C and R-horizons
A - Topsoil B - Subsoil C - Weathered Rock Bedrock
There are typically five soil horizons: O (organic), A (topsoil), E (eluviated), B (subsoil), and C (parent material). Each horizon has unique characteristics and plays a key role in soil composition and function.
The five soil horizons are O horizon (organic matter), A horizon (topsoil), E horizon (eluviated or leached layer), B horizon (subsoil), and C horizon (parent material). These horizons collectively make up the soil profile and influence soil characteristics and fertility.
The correct order of soil horizons, from top to bottom, is O horizon, A horizon, E horizon, B horizon, C horizon, and R horizon. It is important to note that not all soils have all these horizons, as they can vary depending on the specific conditions of the soil.
A stands for top soil.B stands for who knows what and C stands for IDK
a < b < c So, neither a nor b is greater than c.
if a is bigger than b and b is bigger than c a must be bigger than c... Transitivity
horizon a= topsoil horizon b= subsoil i think horizon c im not sure of and then bedrock
NO it is not because if a<b<c it could also be said without the b as a<c.