Abstract
The assessment of irrigation water quality and the study of its negative influence on soil are very important, because the soil salinization is one of the most important ecological problems. Water quality parameters such as pH, TDS, EC, contents of SO4 2−, Cl−, HCO3 −, CO3 2−, Mg2+, Ca2+, Na+ and K+ in Qiala reservoir were determined. This water is used for the irrigation of the soils in Tikanlik oasis. Monthly water sampling was done in 2007. The analysis indicated that major dominant water type was Na+-Cl−. For the classification of irrigation properties of the water the following chemical indices were calculated: sodium absorption ratio, residual sodium carbonate, sodium percentage, permeability index and irrigation coefficient. The classifications of Wilcox and USDA Salinity Laboratory were also used. The analysis of all classification methods have lead us to the conclusion that there was a low possibility of sodium or alkalinity hazard in the soils irrigated by the water of Qiala reservoir but there was a big salinity hazard. This negative influence was also confirmed by IWQI, through calculation of which the various quality indicators of irrigation water were generalized and represented by a single value. The salinization degree of the soils in the 14 different areas of Tikanlik oasis and the dynamics of its changes during the irrigation period were studied as well. During the irrigation period TDS and EC values increased abruptly in the upper soil horizon. All this led to the accumulation of high quantity of salts in the upper soil horizon during the irrigation season. Continuous monitoring of surface water by IWQI is the effective way for the complex assessment of irrigation water quality as well as for the control of the soil salinization process.
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Current research was supported by the CAS (Visiting Fellowship for Researchers from Developing Countries, Grant No. 2013FFZA0010).
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Ghazaryan, K., Chen, Y. Hydrochemical assessment of surface water for irrigation purposes and its influence on soil salinity in Tikanlik oasis, China. Environ Earth Sci 75, 383 (2016). https://doi.org/10.1007/s12665-016-5287-0
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DOI: https://doi.org/10.1007/s12665-016-5287-0