TY  - JOUR
T1  - Rice Irrigation Regimes under the Condition of Kyzylorda Oblast
AU - Bulanbayeva, P. AU - Koshkarov, S. AU - Shayanbekova, B. 
JO  - Research Journal of Applied Sciences
VL  - 15
IS  - 12
SP  - 463
EP  - 470
PY  - 2020
DA  - 2001/08/19
SN  - 1815-932x
DO  - rjasci.2020.463.470
UR  - https://makhillpublications.co/view-article.php?doi=rjasci.2020.463.470
KW  - Rice irrigation system
KW  -drainage network
KW  -soil
KW  -groundwater level
KW  -soil salinization
KW  -water salinity
KW  -rice map
KW  -eco-reclamation conditions
KW  -rice water balance draught
KW  -the thermal regime of water
KW  -salt regime of soils
KW  -irrigation regime
KW  -irrigation rate and filtration coefficient
AB  - 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&deg;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.
ER  - 