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Andisols

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    • CALS
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    • Soil Orders
    • Educator resources
    CALS
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    • Soil Orders
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    1. Home/
    2. CALS/
    3. Soil Orders/
    4. Andisols

    Andisols (from Japanese ando, "black soil") are soils that have formed in volcanic ash or other volcanic ejecta. They differ from those of other orders in that they typically are dominated by glass and short-range-order colloidal weathering products such as allophane, imogolite and ferrihydrite. As a result, Andisols have andic properties — unique chemical and physical properties that include high water-holding capacity and the ability to "fix" (and make unavailable to plants) large quantities of phosphorus. They are divided into eight suborders: Aquands, Gelands, Cryands, Torrands, Xerands, Vitrands, Ustands and Udands.

    Globally, Andisols are the least extensive soil order and only account for approximately 1% of the ice-free land area. They occupy approximately 1.7% of the U.S. land area, including some very productive forests in the Pacific Northwest region.

    1200x900-andisols.jpg
    Andisols have andic soil properties in layers either: (1) with a cumulative thickness of 36 cm within 60 cm of the mineral soil surface; or (2) comprising at least 60% of the depth between the mineral soil surface and a root-restrictive horizon. (USDA-NRCS)

    Soil Orders

    • Alfisols
    • Andisols
    • Aridisols
    • Entisols
    • Gelisols
    • Histosols
    • Inceptisols
    • Mollisols
    • Oxisols
    • Spodosols
    • Ultisols
    • Vertisols

    Xerands, Vitrands (Idaho)

    Xerands — temperate Andisols with very dry summers and moist winters; Vitrands — relatively young Andisols that are coarse-textured and dominated by glass

    Cryands (Iceland)

    Andisols of cold climates

    Vitrands (New Zealand)

    Relatively young Andisols that are coarse-textured and dominated by glass

    Udands (Costa Rica)

    Andisols of humid climates

    Andic soil properties, Mazama eruption

    Andic soil properties are characteristic of Andisols, soils formed from volcanic ash, which are significantly influenced by the Mount Mazama eruption (~7,700 years ago) in the Pacific Northwest

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    Soil Orders

    • Alfisols
    • Andisols
    • Aridisols
    • Entisols
    • Gelisols
    • Histosols
    • Inceptisols
    • Mollisols
    • Oxisols
    • Spodosols
    • Ultisols
    • Vertisols

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    Department of Soil and Water Systems

    Email: rheinse@uidaho.edu
    Location: E. J. Iddings Agricultural Science Laboratory, Rm 242; 606 S Rayburn St
    Mailing Address:

    875 Perimeter Drive MS 2340
    Moscow, ID 83844-2340

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