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In the Arctic ecozone, the predominant soil types are predominantly gelisols, characterized by permafrost layers that impede drainage and lead to unique hydrology. These soils often contain a mix of organic material and mineral matter, resulting in a cold, nutrient-poor environment. Additionally, tundra soils, which can be classified as histosols, are rich in organic material due to slow decomposition rates in the cold climate. The harsh conditions limit soil development, leading to thin and poorly developed horizons.

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2mo ago

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