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7.8.2: Sodic Soils

  • Page ID
    44437
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    The reclamation of sodic soil usually requires that water penetration into and through the soil be improved by either exchanging excess sodium in the soil with calcium, so that leaching can proceed or by initially leaching with saline water, and then by progressively decreasing the salinity of the applied water. If the choice is to replace sodium with calcium, then an amendment must be applied that either contains soluble calcium or dissolves calcium already present in the soil. Examples of amendments that contain calcium are gypsum, lime, and calcium chloride. Sulfur, sulfuric acid, and pyrite are examples of amendments that will react and dissolve calcium present in the soil. Occasionally, calcium present in the subsoil can be mixed with a shallow sodic layer by deep tillage, thus, eliminating or reducing the need for an amendment.

    Successive dilutions of a high salt water containing calcium can be an effective method of reclaiming sodic soil. The basic requirement is an adequate supply of a high saline water and a low salinity water. After initially applying the highly saline water, this water is diluted in steps with the low salinity water until only the low salinity water is applied and the reclamation process is complete.

    Tillage to create a rough, yet thoroughly disturbed, soil surface is a common practice for improving water infiltration. Typically, a sodic soil is tilled prior to each intermittent water application during reclamation.


    7.8.2: Sodic Soils is shared under a CC BY-NC-ND 4.0 license and was authored, remixed, and/or curated by LibreTexts.