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تأثير نوعية مياه الري وبعض محسنات التربة في خواص التربة وإنتاجية محاصيل العلف في ظروف حوض الفرات الأدنى

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 Publication date 2010
and research's language is العربية
 Created by Shamra Editor




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References used
غزال حسن 1990تربية المحاصيل جامعة حلب - مديرية الكتب والمطبوعات
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This experiment was conducted during ١٩٩٦-١٩٩٨ to ivestigate study the effect of using different types of irrigation water on some soil properties and its cotton, corn and wheat productivity under the agroclimatic conditions of Deir Ezzor.
The provision of adequate drainage and the accompanying problem of accumulation of salt in soil have plagued irrigated agriculture for centuries. Soil salinity is one of the major problems in arid and semi-arid zones. In Euphrates valley the high groundwater level and its high evaporation rate caused a serious salinity problem. This study was aimed to allocate the dangerous areas in terms of high water level resulted from the recent and expected activities. Drainage wells will be drilled at these areas in order to lower the groundwater level and prevent further soil salinity.
The purpose of this research is to apply a mathematical program to calculate water and chemical balance in unsaturated soils, under the influence of different methods of irrigation, in order to monitor the amount of vertical drainage of water insi de the soil and choose a irrigation method that can reduce the phenomenon of groundwater pollution. Three irrigation methods were tested with different fertilization method. The study was conducted in the western part of Homs Governorate (AlQusair orchards).
Sector No. 5 is located on the right side of Euphrates River, Southeast of ALMyadeen City. Many lands there are not suitable for agricultural uses, because of the saline soils. This research aimed to evaluate the system of the unconfined groundwate r resources, by adopting the measurement results in 40 piezometers, drilled in aquifer of quaternary deposits which consist of loam, gravel, and sandy gravel, underneath which are impervious Neogene deposits. The annual changes of groundwater levels of quaternary aquifer were 1-3 meters, due to rain and irrigation water leaking. The groundwater table is shallow (less than 2.5 m), because of the excessive irrigation, which gives an urgent necessity to construct effective drain network to reduce groundwater levels. Groundwater salinity reaches 29 gr/liter, and concentrations of the chloride and sulphate are 11 gr/liter, 3,5 gr/liter in some locations, because of the natural and artificial situations. Therefore, this groundwater is not suitable for domestic, or agricultural purposes in most areas of the region.

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