| Project Manager | A.R. Ramazanov, SPA SANIIRI The Republic of Uzbekistan, 700187, Tashkent, Karasu-4/11 | 
                
                  | Summary | Investigations on improvement of water use 
                    and soil water-salt regime management, irrigated lands productivity 
                    increase were carried out in the rice sowing zone of Amudarya 
                    low reaches. Territory is located in the North of AmuDarya 
                    delta and presented mostly by strongly saline meadow-desert 
                    soils. Soils made of clay, loam, clayey sand and sand. Climate is sharply continental. Before rice irrigation systems construction 
                    the ground waters with mineralization 0.3-30 g/l were at 
                    a depth of 3 -10 m. Experimental Production Plot area is 
                    45 ha. Land use efficiency is 0.71 - 0.83. Over the plot 
                    territory the gauging stations, observation wells and piezometers  
                    are installed. Instrumental survey of  canals and distribution 
                    network and salt survey were  conducted. After 4-years rice 
                    irrigation the salt content in thickness 0 - 3m was 0.23 
                    - 0.42 % and 0.02 -0.07 % - on chlorine-ion. Salt balance 
                    of aeration zone was of desalination type. Under basic mineralization 
                    of ground water 18.6 - 44,6 g/l after second year of  irrigation it decreased to 7 - 22.8 g/l. At the end 
                        of vegetation after 4-year rice cultivation the ground water 
                        mineralization was within 7.2 -11.2 g/l. Significant salt 
                        quantity from rice irrigation systems territory is removed 
                        by drainage outflow. Minimum value of drainage water mineralization 
                        (0.76 - 3.22 g/l) was noted in the period of water release 
                        from rice fields (June-September). After water release from 
                        rice fields at the end of vegetation the salt content in 
                        drainage outflow increases (9.49 -11.89 g/l) that is due 
                        its formation by inflow from distribution network and saline 
                        ground water. Moisture content in thickness 0 - 40 cm before 
                        rice sowing was 15,65 % (first year);  14,4 % (fifth year); 
                        in thickness 40 -100cm - 22,4 and 24,1 % from soil weight  
                        accordingly. After rice harvest it was 25,0 -23,8 (0 -40 
                        cm) and 27,3 -24.1 %  (40 -100 cm). In the thickness 100 
                        -150cm soil moisture was 22,8 -24,0 %  (spring) and 27,5 
                        -26,5 % (autumn). | 
                
                  | Bibliography | 1. Authors: A.R.Ramazanov, A.R. Kurbanbayev, Kh.I. 
                    YakubovTitle: Some issues of Amudarya low uppers reclamation  
                    Nukus, "Karakalpakstan", 1978 Monograph includes main results of ecologic-reclamation 
                        process research under different crops irrigation development 
                        and presents technical and technological recommendations 
                        on their management. |