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Soil · Soil type

Saline Soil

Also known as: Salt-affected soil, Salinized soil

Saline soil contains elevated levels of soluble salts in the soil solution, raising osmotic stress on plant roots and reducing water availability even when soil moisture is present. It commonly develops in arid and semi-arid regions, poorly drained land, and irrigated areas with inadequate leaching or drainage.

Dated referenceLast reviewed: 2026-07-12Updated: 2026-07-12
Salt-affected soil
MODIS Land Rapid Response Team, NASA GSFC, via Wikimedia Commons (Public domain) Public domain (opens in a new tab) source (opens in a new tab)Downloaded from Wikimedia Commons; resized to a maximum width of 1280 px and recompressed as JPEG for web delivery. Content unaltered.

Soil salinity is measured by the electrical conductivity (EC) of the soil solution, which rises with the concentration of soluble salts. Saline soils occur naturally in arid and semi-arid regions where evaporation exceeds rainfall and salts are not leached away, and can also develop or intensify through human activity, particularly irrigation with saline water or insufficient drainage.

Saline soils are related to, but distinct from, sodic soils, in which high exchangeable sodium causes structural breakdown rather than primarily osmotic stress; some soils are affected by both conditions together. High soluble salt content can occur across any texture class, though poor drainage in fine-textured soils often makes salinity harder to manage.

Overview

Salinity is defined by the concentration of soluble salts in the soil solution rather than by texture, and can develop on almost any soil type given the right combination of climate, drainage, and water source. It is distinct from, though sometimes associated with, sodic soils, where high exchangeable sodium causes structural rather than primarily osmotic problems.

Physical and chemical properties

Osmotic effect
High salt concentration in the soil solution reduces the ability of roots to draw in water, even when soil moisture content appears adequate.
Ion toxicity
Specific ions such as sodium or chloride can be directly toxic to sensitive crops at high concentrations.
Drainage interaction
Poor drainage concentrates salts near the surface through evaporation and capillary rise, especially in low-lying or fine-textured soils.
Texture independence
Salinity can occur in soils of any texture class; the underlying cause is the salt content of the soil solution, not the mineral particles themselves.

Management considerations

Managing saline soils centres on moving salts below the root zone and preventing their re-accumulation, alongside matching crop choice to the salinity level present.

  • Improve drainage to allow leaching of salts below the root zone
  • Where water supply and drainage allow, apply enough water beyond crop needs to leach accumulated salts
  • Select salt-tolerant crops or varieties suited to the local salinity level
  • Where sodium accumulation is also a factor, gypsum applications are a common reclamation tool used under local agronomic guidance

Crop suitability

Barley is among the more salt-tolerant cereal crops and is commonly grown on moderately saline soils. Sugar beet is also relatively salt-tolerant. Many other crops are considerably more sensitive and can suffer yield loss at salinity levels that barley or sugar beet tolerate well.

Assessing a saline soil

Soil salinity is assessed through laboratory testing of electrical conductivity, typically from a saturated paste extract or a standard soil-to-water extract. Local extension services or accredited soil laboratories provide the most reliable testing and interpretation for a given crop and region.

Relationships

Evidence-backed connections in the knowledge graph.

Scope & limitations

Geographic scope: General soil-science overview of salt-affected soils occurring in arid and semi-arid regions worldwide and in some irrigated or poorly drained lowlands; salinity levels and causes vary greatly by location.

Climate context: Most prevalent in arid and semi-arid climates where evaporation exceeds rainfall, concentrating salts at or near the surface; irrigation without adequate drainage can produce similar effects in wetter climates.

  • Salinity severity and appropriate crop or management thresholds vary by soil, water source, and local climate; this overview does not substitute for site-specific soil and water testing.
  • Sodic soils, involving high exchangeable sodium and structural breakdown, are a related but distinct condition that may require different management.

Sources

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

  1. [1]USDA NRCS — Natural Resources Conservation Service (opens in a new tab)

    USDA Natural Resources Conservation Service (NRCS)

    Authoritative

    Cited for: Soil texture, drainage, and management

    Type:
    Government agency
    Jurisdiction:
    United States
    Accessed:
    2026-07-12
  2. [2]FAO — Soils Portal (opens in a new tab)

    FAO Global Soil Partnership

    Authoritative

    Cited for: Soil function and classification context

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

    Cited for: Global soil properties and information

    Type:
    Research institute
    Jurisdiction:
    Global
    Accessed:
    2026-07-12
  4. [4]FAO — Land and Water (opens in a new tab)

    FAO Land and Water Division

    Authoritative

    Cited for: Salinity, drainage, and irrigation water management

    Type:
    Intergovernmental organization
    Jurisdiction:
    Global
    Accessed:
    2026-07-12