A soil scientist collects core samples from a mature, undisturbed forest soil profile to analyze its vertical stratification. Order the standard soil horizons sequentially from the uppermost surface layer down to the partially weathered parent material.
- 1O Horizon: A surface layer consisting primarily of newly deposited and decomposing organic litter such as leaves and twigs.
- 2A Horizon (Topsoil): A mineral-rich layer mixed with thoroughly decomposed dark organic matter (humus) with high biological activity.
- 3B Horizon (Subsoil): A zone of accumulation (illuviation) where leached minerals, clays, and iron oxides collect.
- 4C Horizon: A layer composed of partially weathered and mechanically broken bedrock fragments with minimal organic influence.
Cevap
The correct sequence from surface to depth is the O Horizon (surface organic litter), followed by the A Horizon (topsoil), the B Horizon (subsoil zone of accumulation), and finally the C Horizon (partially weathered parent material).
In a well-developed soil profile, soil develops in distinct horizontal layers known as horizons from the surface down to bedrock. The correct sequence starts at the surface with the organic O Horizon, descends into the mineral-rich A Horizon (topsoil), continues into the B Horizon (subsoil/illuviation zone), and terminates at the C Horizon (partially weathered parent material).
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Anahtar Kavram
Vertical soil horizon stratification in a mature soil profile
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