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Soil · Soil type

Ferralsol

Also known as: Oxisol (USDA), Deeply weathered tropical soil

A Ferralsol is a deep, intensely weathered tropical soil dominated by iron and aluminium oxides and low-activity clays. It typically has good physical structure and drainage but low natural fertility, high phosphorus fixation, and acidity, so productive use depends heavily on nutrient and acidity management.

Dated referenceLast reviewed: 2026-07-13Updated: 2026-07-13
Illustrative diagram · AgricultureID (original)

Ferralsols are among the most intensely weathered soils on Earth, formed over long periods in warm, humid tropical climates where prolonged weathering and leaching have removed most soluble minerals and weatherable material. What remains is dominated by iron and aluminium oxides and by low-activity clays, giving the soils their often red or yellow colours and their characteristic chemical poverty.

Despite this chemical poverty, Ferralsols frequently have favourable physical properties: they are typically deep, well drained, and strongly aggregated, so that a clayey soil can feel friable and stable. Their agricultural challenge is therefore chemical rather than physical, centred on low nutrient reserves, strong fixation of phosphorus by the oxides, acidity, and sometimes aluminium toxicity, all of which must be managed for sustained production.

Overview

A Ferralsol is defined by extreme weathering: a deep, uniform, oxide-rich subsoil in which most weatherable minerals and soluble nutrients have long since been removed. The dominance of iron and aluminium oxides gives strong, water-stable aggregates and vivid red or yellow colours, but also the low nutrient-holding capacity that limits fertility.

Formation and distribution

Ferralsols form on old, stable land surfaces in the humid tropics, where high temperatures and abundant rainfall drive intense chemical weathering and leaching over very long periods. This progressively strips out silica and base cations, concentrating resistant iron and aluminium oxides. They are extensive in the humid tropics of South America, notably the Brazilian and Amazonian uplands, and of central Africa, with occurrences in parts of tropical Asia.

Physical and chemical properties

Oxide dominance
Iron and aluminium oxides dominate the mineralogy, producing red and yellow colours and stable aggregates.
Low fertility
Low-activity clays give a small cation exchange capacity and poor retention of nutrients, so natural fertility is low.
Phosphorus fixation
The oxides strongly bind phosphorus, so applied phosphate can become largely unavailable to crops.
Good structure and drainage
Strong aggregation gives friable, well-drained, physically stable soil despite a high clay content.

Management considerations

Sustaining crops on Ferralsols depends on overcoming their chemical limitations while conserving the organic matter and structure that hold the system together.

  • Manage acidity with lime and address possible aluminium toxicity to allow sensitive crops to root
  • Supply phosphorus carefully, recognising that much can be fixed by the oxides, and use efficient placement
  • Maintain organic matter and continuous cover to protect the small nutrient reserve and prevent erosion
  • Favour perennial and deep-rooting crops and agroforestry, which suit the deep, well-drained profile and recycle nutrients

Crop suitability

With appropriate management, Ferralsols support important tropical crops, especially those tolerant of low fertility and acidity or grown as perennials that recycle nutrients. Cassava is well adapted to these soils, and oil palm, coffee, rubber, and pineapple are widely grown on Ferralsols across the humid tropics.

Relationships

Evidence-backed connections in the knowledge graph.

Scope & limitations

Geographic scope: Humid tropics worldwide, extensively in South America and central Africa; properties reflect intense weathering but vary with parent material, age, and management.

Climate context: Ferralsols are products of warm, humid tropical climates, where high temperatures and heavy rainfall drive the prolonged weathering and leaching that create their deep, oxide-rich, nutrient-poor profiles.

  • Natural fertility is low and phosphorus is strongly fixed, so sustained cropping depends on careful nutrient and acidity management.
  • Fertility gained after clearing native vegetation can decline quickly if organic matter and cover are not maintained.
  • This entry is a general overview; acidity, aluminium, and nutrient status should be confirmed by local soil testing.

Sources

This article draws on the following authoritative sources. See our sources & methodology for how they are selected.

  1. [1]FAO — Soils Portal (opens in a new tab)

    FAO Global Soil Partnership

    Authoritative

    Cited for: Ferralsol Reference Soil Group, weathering, and distribution

    Type:
    Intergovernmental organization
    Jurisdiction:
    Global
    Accessed:
    2026-07-12
  2. High

    Cited for: Global information on Ferralsols and highly weathered soils

    Type:
    Research institute
    Jurisdiction:
    Global
    Accessed:
    2026-07-12
  3. [3]USDA NRCS — Natural Resources Conservation Service (opens in a new tab)

    USDA Natural Resources Conservation Service (NRCS)

    Authoritative

    Cited for: Oxisols, phosphorus fixation, and acidity management

    Type:
    Government agency
    Jurisdiction:
    United States
    Accessed:
    2026-07-12
  4. [4]IITA — CGIAR research center (tropical crop breeding) (opens in a new tab)

    International Institute of Tropical Agriculture (IITA)

    High

    Cited for: Management of weathered tropical soils for crops

    Type:
    Research institute
    Jurisdiction:
    Sub-Saharan Africa / Global
    Accessed:
    2026-07-12