diagnostic horizon
Quick Summary
In pedology, a diagnostic horizon is a key concept used for classifying soils. These horizons are defined by the specific types of accumulated weathering products they contain, such as clay, mixtures of iron oxides and humus, or soluble salts. They can also be characterized by the presence of a hard, impermeable layer, like an indurated calcium carbonate or iron-rich layer.1
Soil horizons are distinct layers within the soil profile, formed by the actions of organisms and percolating water. From the surface downward, common horizons include O (organic matter), A (humus accumulation), E (leached, bleached appearance), B (accumulation of material from upper layers), C (unweathered parent material), and R (bedrock). Diagnostic horizons are crucial for understanding soil properties and classification.12
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