@article{MAKHILLRJAS2020151210275,
    title = {Rice Irrigation Regimes under the Condition of Kyzylorda Oblast},
    journal = {Research Journal of Applied Sciences},
    volume = {15},
    number = {12},
    pages = {463-470},
    year = {2020},
    issn = {1815-932x},
    doi = {rjasci.2020.463.470},
    url = {https://makhillpublications.co/view-article.php?issn=1815-932x&doi=rjasci.2020.463.470},
    author = {P.,S. and},
    keywords = {Rice irrigation system,drainage network,soil,groundwater level,soil salinization,water salinity,rice map,eco-reclamation conditions,rice water balance draught,the thermal regime of water,salt regime of soils,irrigation regime,irrigation rate and filtration coefficient},
    abstract = {Keeping up 12-15 cm layer of water in a rice
draught in the post-tilling to waxen ripeness does not
provide a favorable thermal and saline soil and water
regimes. Temperature regime of water in a rice draught is
determined by climatic conditions of the region and the
depth of water on crops. In conditions of extreme
continental climate of Syr-Darya water layer at a depth of
12-15 cm in the water warms up the draught 31,0 - 32,5°C
which negatively affects the growth and development of
rice plants and its yield. Favorable thermal regime of
water is observed at a depth of 17-22 cm and here we
have the necessary salt regime of irrigated soils.
Therefore, maintaining the draught in paddy water layer
depth of 17-22 cm provides favorable salt and thermal
regimes of water and soil.}
    }