يتضمن هذا البحث دراسة احتمال انهيار سد كودنه الذي يقع على وادي الرقاد في محافظة
القنيطرة، حيث تًم تسليط الضوء على مفهوم انهيارات السدود و أشكال فتحة الانهيار فيها
باستخدام برنامج الhec-ras, كما تضمن هذا البحث مناقشة بعض سيناريوهات الانهيار ،
و اختيار السيناريو الأخطر حيث استطاع تحديد زمن وصول الموجة الفيضانية إلى كل مقطع
عرضي.
This research involves the study of collapse's possibility of Codana dam,
which is located on Al-Rakad valley in Quneitra governorate. The light had
been shed on: the concept of dam's collapse, forms of collapse slots by using
Hec-Ras program, Also it had been shown the reliable collapse scenarios and
choose the worst one when the access time of flood wave could be identified
for every cross-section.
References used
BRUNER.G, 2010- HEC-RAS User's Manual. CPD-68, p 790
WAHL, T. 1998 -Prediction of Embankment Dam Breach Parameters. U.S. Department of the Interior, p.72
CAMERON. T, ACKERMAN. P, May 2012 -Hec-GeoRas GIS Tools for Support of Hec-Ras using ArcGIS 10. User's Manual, CPD-83, p520
Thousands of dams have been built around the world, but, the date of construction is
associated with a history of failures and collapse, due to the high water levels, generating
higher returns consequences disastrous for the environment and society
This research aims to check the actual performance of the work of the propeller
depending on series of results issued from Hamburg basins that are known by RANSE
where the arcs analysis and the hydrodynamic characteristics of the propeller work in
The goal of this work is finding exact solitary wave solutions to generalized Fitzhug-Nagumo equation with constant coefficients, by using the exp-function method, where we have illustrated graphically one of them, the obtained results, with aid of s
This research is concerned in modeling the problem of sloshing in
moving cylindrical containers in ANSYS program where we model
the problem on a partially filled cylinder then we find the resonant
frequencies in addition to study the interaction between the cylinder
and the fluid.
Joints study in Skhaba region shows the existence two joint directions, principal dominant
NW-SE Joints from extension origin upper Cretaceous age, unrelated and older than faults
in studied area statistically, the presence of Calcareous filling in