词条 | Alfisol |
释义 | Alfisol soil type ![]() Alfisols typically exhibit well-developed, contrasting soil horizons (horizon) (layers) depleted in calcium carbonate but enriched in aluminum- and iron-bearing minerals. Below the surface horizon lies a region with significant accumulation of translocated (migrated) layer silicate clay. This region, called the argillic horizon, is characterized by a relatively high content of available calcium, magnesium, potassium, and sodium ions. Alfisols are lower in humus content than Mollisols (Mollisol) (a similar soil order) and do not have the calcium carbonate accumulation of that soil type. They are less extensively leached of metal ions and develop in cooler climates than the Ultisols (Ultisol), a clay-rich soil order of warmer regions. |
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