Abstract

The work deals with the study of hydromorphology of the regulating lake which located at (50Km) north of Mosul city. The survey started in November, 2012 using the EchoSounder, and carried out by dividing the lake into (30) sections starting from the lower surface of the main dam and ending at the regulating dam. Data are recorded and represented using GIS technology (Arc GIs v10.4) and Microsoft program (Excel). The survey shows that the shallowest depth in the lake is found at left bank of section (5) which reached (7.65 m) and the deepest point is Found in the left bank of the section (9) which reached (18.22m) directly on the Thalwage line. The hydraulic gradient of the lake is (1m/Km ), and the overall shape of the sections is (U) shape. The variation in depth in each section is mostly due to difference in the sedimentation and erosion. There was deposition on the convex sides and erosion in the concave sides of the banks, the erosion and sedimentation processes vary with the variation of water velocity, slope and rock components of the river along the regulating lake.

Highlights

  • ‫‪The work deals with the study of hydromorphology of the regulating lake which‬‬ ‫‪located at (50Km) north of Mosul city

  • The survey started in November, 2012 using‬‬ ‫‪the EchoSounder, and carried out by dividing the lake into (30) sections starting from‬‬ ‫‪the lower surface of the main dam and ending at the regulating dam

  • ‫‪The survey shows that the shallowest depth in the lake is found at left bank of‬‬ ‫‪section (5) which reached (7.65 m) and the deepest point is Found in the left bank of‬‬

Read more

Summary

Introduction

‫‪The work deals with the study of hydromorphology of the regulating lake which‬‬ ‫‪located at (50Km) north of Mosul city.

Results
Conclusion

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.