Saad,, A. (2003). EFFECTS OF SALINE WATER FLUX ON CHANGES I EFFLUENT QUALITY, LEACHING FRACTION, EVAPO - ATION AND SALT LOAD IN COARSE - TEXTURED SOIL. Journal of Soil Sciences and Agricultural Engineering, 28(8), 6517-6530. doi: 10.21608/jssae.2003.245100
A. F. Saad,. "EFFECTS OF SALINE WATER FLUX ON CHANGES I EFFLUENT QUALITY, LEACHING FRACTION, EVAPO - ATION AND SALT LOAD IN COARSE - TEXTURED SOIL". Journal of Soil Sciences and Agricultural Engineering, 28, 8, 2003, 6517-6530. doi: 10.21608/jssae.2003.245100
Saad,, A. (2003). 'EFFECTS OF SALINE WATER FLUX ON CHANGES I EFFLUENT QUALITY, LEACHING FRACTION, EVAPO - ATION AND SALT LOAD IN COARSE - TEXTURED SOIL', Journal of Soil Sciences and Agricultural Engineering, 28(8), pp. 6517-6530. doi: 10.21608/jssae.2003.245100
Saad,, A. EFFECTS OF SALINE WATER FLUX ON CHANGES I EFFLUENT QUALITY, LEACHING FRACTION, EVAPO - ATION AND SALT LOAD IN COARSE - TEXTURED SOIL. Journal of Soil Sciences and Agricultural Engineering, 2003; 28(8): 6517-6530. doi: 10.21608/jssae.2003.245100
EFFECTS OF SALINE WATER FLUX ON CHANGES I EFFLUENT QUALITY, LEACHING FRACTION, EVAPO - ATION AND SALT LOAD IN COARSE - TEXTURED SOIL
Dept., of Soil and Water Sci., Fac. of Agrlc., Eishatby, Unlv. of Alex.
Abstract
TwO laboratory experiments were conducted on sandy soil columns tp quantity the dynamic changes of effluent salinity (Ee) and sodium adsorption ratip (SAR) as well as leaching fraction (IF) and salt load as a result of using water with E<i: 0.5. 1.2.1.8.2.37. and 3.6 dS.m·'. Downward Aux simulates normal surlace irrigatio while upward flux simulates subsurface irrigation. The results indicated Ihat (herr were polynomial relationships between EC and SAR of leachate and elF) and lim! when the EC values of applied mixing water were> 0.5 ds.m". Exponential relation between EC. SAR and IF wilh time were obtained when the EC of applied water wa 0.5 dS.m·l. Linear regression equations between the cumulative evaporation and the lime of upward nux were obtained under different salinity levels of applied water. The contribution of upward and downward saline water to build up salt load in soil column$ was clear. The maximum values of osmotic potential in the surface layer were 0.83 and 0.58 bar as 8 result of upward and downward nux of saline water (3.6 dS.m·\ respectively. Thus the adverse effects on soil properties as a result of increased salt concentration can be minimized by controlling the mixing ratio. It was concluded that the use of poor quality water in irrigalion. particularly in coarse - textured soil. becomes an efficient means in a scare resource without risks due to mismanagement this requires appropriate sa Unity by mixing agricultural drainage water with canal water. Best soil and water management practices and aoequate leaching are also required 10 keep suitable sail balance in a given soil depth. I
View on SCiNiTO
Top