Amelioration of calcareous saline sodic soils through phytoremediation and chemical strategies

Abstract

Abstract. The worldwide occurrence of saline sodic and sodic soils on more than half a billion hectares warrants attention for their efficient, inexpensive and environmentally acceptable management. These soils can be ameliorated by providing a source of calcium (Ca2+) to replace excess sodium (Na+) from the cation exchange sites. Although chemical amendments have long been used to ameliorate such soils, the chemical process has become costly during the last two decades in several developing countries. As a low‐cost and environmentally acceptable strategy, the cultivation of certain salt tolerant forage species on calcareous sodic and saline sodic soils, i.e. phytoremediation, has gained interest among scientists and farmers in recent years. In a field study conducted at three calcareous saline sodic sites (pHs=8.1–8.8, ECe=7.8–12.5 dS m–1, SAR=30.6–76.1) in the Indus Plains of Pakistan, we compared chemical and phytoremediation methods. There were four treatments; two involved plants: Kallar grass (Leptochloa fusca (L.) Kunth), and sesbania (Sesbania bispinosa (Jacq.) W. Wight). The other two treatments were uncropped: soil application of gypsum and an untreated control. All treatments were irrigated with canal water (EC=0.22–0.28 dS m–1). The plant species were grown for one season (5–6 months). Sesbania produced more forage yield (34 t ha–1) than Kallar grass (23 t ha–1). Phytoremediation and chemical treatments resulted in similar decreases in soil salinity and sodicity, indicating that phytoremediation may replace or supplement the more costly chemical approach. The soil amelioration potential of sesbania was similar to that of the Kallar grass, which suggests that moderately saline sodic calcareous soils can be improved by growing a forage legume with market value.

Using HYDRUS to simulate the dynamic changes of Ca²⁺ and Na⁺ in sodic soils reclaimed by gypsum

“…At the same time, the Ca 2+ in the supplied water will react with the sodic salts in the soil solution and the exchangeable sodium in the soil colloid, which will consume a portion of the Ca 2+ in the soil solution (Qadir et al 2002;. Although the Ca 2+ in the supplied water did not supply this soil layer, the Ca 2+ in this soil layer penetrates to the soil layer underneath.…”

Sodium-resistant plant growth-promoting rhizobacteria isolated from a halophyte, Salsola grandis, in saline-alkaline soils of Turkey

“…Phytoremediation has attracted rising attention as a suitable technology that can be applied not only in polluted but also in saline soil remediation because of its low economic cost and environmentally friendly process (Qadir et al, 2002(Qadir et al, , 2003. Some reports suggest that the harvested plant, if not plowed back to the same soil, can contribute significantly to the removal of salts such as sodium (Na) from salt-affected soils (Ravindrana et al, 2007;Qadir et al, 2007).…”

Assimilation and Translocation of Dry Matter and Phosphorus in Rice Genotypes Affected by Salt-Alkaline Stress

“…Although the inorganic phosphorus content in crops is generally low, it plays an important role in stabilizing the pH and metabolic balance of the cellular protoplasm [44]. The low Ca-P mineral solubility and ionic competition with H 2 PO 4´a nd HPO 4 2´s everely restricted the availability of phosphorus in salt-alkaline soils [45].…”