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Influence of water table fluctuation in the tail of drains and irrigation canals on chemical and physical properties of soil in the north Nile delta region [electronic resources].

By:

Abo Waly, M. E

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Language: English Summary language: Arabic Description: p.111-124Other title:

اثر تذبذب مستوى الماء الارضي بنهايات الترع والمصارف على خواص التربه الطبيعيه والكيميائيه فى منطقة شمال دلتا النيل [Added title page title]

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Mansoura University Journal of soil sciences and agricultural engineering, 20112 v. 3 (1) [electronic resources].

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In: Mansoura University Journal of Soil Sciences and Agirucultural Engineering 2012.v.3(1)Summary: The objectives of the present study were to determine the fluctuation effect of water table level in tail ends of drains and irrigation canal on chemical and physicai properties of the soil in North Nile Delta region. Six soil profiles from Kafr EI-Sheikh were excavated at each location in two lines under investigation. The studied area is located between EL-Gharbia main drain and Nashart drain, since it was started from Kafr El-Sheikh towards the Mediterranean Sea in the north for the first line. Three locations were chosen on Nashart drain at a distance of 5, 10 and 20 km from Burullus Lake towards Sedi-Salim district. The second line of study was EL-Gharbia main drain. Three locations were selected on a distance of 5, 20 and 30 km from the sea towards Kafr- EI-Sheikh city. Three observation wells at 10, 50 and 100 meters distance for each profile were installed and the fluctuation of water table depths were recorded. table fluctuation of water were recorded.

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The objectives of the present study were to determine the fluctuation effect of water table level in tail ends of drains and irrigation canal on chemical and physicai properties of the soil in North Nile Delta region. Six soil profiles from Kafr EI-Sheikh were excavated at each location in two lines under investigation. The studied area is located between EL-Gharbia main drain and Nashart drain, since it was started from Kafr El-Sheikh towards the Mediterranean Sea in the north for the first line. Three locations were chosen on Nashart drain at a distance of 5, 10 and 20 km from Burullus Lake towards Sedi-Salim district. The second line of study was EL-Gharbia main drain. Three locations were selected on a distance of 5, 20 and 30 km from the sea towards Kafr- EI-Sheikh city. Three observation wells at 10, 50 and 100 meters distance for each profile were installed and the fluctuation of water table depths were recorded. table fluctuation of water were recorded.

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