Oxisols are highly weathered tropical soils characterized by a deep subsurface horizon dominated by iron and aluminum oxides. They form under rainforest vegetation in areas with high rainfall and warm temperatures, causing intense chemical weathering that leaches most nutrients from the soil. Oxisols occupy about 8% of the world's land area, mostly in central Africa, northern South America, and southeast Asia. They require careful management and fertilization due to low fertility resulting from the weathering process.