|  
          
          FEATURES 
            OF SOIL WATER-SALT REGIME IN AN ARID ZONE Arid 
            zones are characterized of high dryness of the climate, and irrigation 
            is economically justified actually for all crops. Demands of the crops 
            to regime of moisture and salts in the root-existing layer (which 
            changes as well with plants' growth) considerably vary over a vegetative 
            period. These demands can be assigned in the form of a certain range 
            of permissible values of moisture and salt concentration in the soil's 
            active layer which increases with growth of plants, at those crops 
            can normally develop. Since water and salt regimes of soils are formed through a series 
            of factors, it is very complicated to forecast these regimes for long 
            periods without specific computations. Nevertheless, available materials 
            of investigations, analyses, modeling of the phenomenon enable qualitative 
            and quantitative forecasting; this question will be considered in 
            the next sections.
 As to an arid zone, we can say with all evidence that to meet agro-technical 
            demands of plants, one have to solve contradictory, per se, task: 
            how to feed a field with required water amount with minimum introduction 
            of salts, and how to withdraw maximum salts out off the field with 
            minimum water drainage. This is the main feature of soil water-salt 
            regime in an arid zone, solution of which lies in the range of irrigation 
            regime optimization and improvement of the irrigation systems in the 
            whole. Availability of relatively simple models allowing carrying 
            out of numerical experiments offers interesting challenges for perception 
            of regularities of forming irrigated soil's water-salt regime. Appearance 
            in the calculations, in addition to soil moisture assessment, of the 
            second factor - salinity (more truly, concentration of soil solution) 
            allows designating a new concept - soil moisture quality, making specified 
            at that the wide-used concept - accessibility of soil moisture. This, 
            as shown in the "Examples of 
            using water-salt regime models" section, open up 
            possibilities, at first, for rational planning of water resources 
            use in a specific water situation; at second, allows making forecasts 
            and analyzing consequences of one or other design decisions; and, 
            at third, enable targeted planning of expensive field, and especially, 
            long-term experiments for confirming or elaborating items of the forecast 
            and, thus, of the models.
 Probably, the most interesting, relatively "unexpected" 
            conclusion is drawn from a series of numerical experiments that should 
            be verified by an experimental way; this consists in possibility of 
            actually equivalent (by efficiency) using irrigation water in spring-autumn 
            instead of that in summer, that is conduction of a part of vegetative 
            irrigation during a non-vegetation period without crop yield losses 
            owing to improvement of soil moisture quality by the vegetative period. 
            This, taking into consideration the current situation with energetic 
            operation mode of the Toctogul reservoir, the major regulator of the 
            tandem reservoir system for long-term regulation of the Syrdarya river 
            flow, is one of the alternatives for way-out of the critical situation 
            have been developed last years. See the " 
            On moisture-charging irrigation's roles in increasing water supply 
            to irrigated lands ".
 As well forecasts of irrigation water expenditures under different 
            conditions of draining a territory are interesting. On the picture, 
            the results of forecasting the net irrigation rate value for different 
            drainage degree are shown. If one considers those without taking onto 
            account water losses on fields because of an imperfect irrigation 
            technique, then it may seem that they contradict the practice; and 
            if one analyzes the situation more carefully, considering the data 
            of independent experiments, then so interesting ideas occur that they, 
            in the author's opinion, may be crucial when selecting means and directions 
            for settlement of the critical situation in CAR.
 Perfect 
            irrigation technique can solve problems concerning lack of water resources 
            and, at the same time, answer the question - "what to do with 
            the salts". By the way, the American water specialists for many 
            years have been professed and put into effect similar ideas in their 
            country (T.V.Belyaeva).
  
            How 
            to get in touch with us? Return 
            to the main pag |