Title : Sustainable management of sodic water irrigated arid soils: Issues and strategies
Abstract:
The farming system in arid region of Rajasthan (India, rainfall zone of 200- 250 mm) in mainly rainfed but in pockets brackish ground water occurs, which is commonly used for irrigation. Brackish water, characterized by low calcium, magnesium and sulphate ions and high sodium, carbonate and bicarbonate ions and high residual sodium carbonate (RSC) create sodicity in soil. Internationally, water containing RSC more than 2 m moles L-1 (Eaton, 1950; Wilcox et al. 1954) and in arid Rajasthan RSC more than 5 m moles L-1 (Joshi and Dhir, 1989) has been considered unsafe for irrigation. Irrigation with water of higher RSC (10- 20 m moles L-1) and high sodium adsorption ratio (SAR 20-35) and moderate salinity (3.5- 4.6 dSm-1 ) causes severe sodicity in soil resulting in development of alkalinity pH (9.2- 10.5) and high exchangeable sodium percent (40-50) in soils.