Abstract

Blocking of diversion intakes and canals by sediment deposition is a widespread problem in many spate irrigation (flood water farming) systems. In the Gash Spate Irrigation Scheme (GSIS), particularly the Fota block, sedimentation is a continuous challenge that resulted in 75% reduction of the irrigable land (2012 data). The scheme receives sediment laden flood water from the Gash River which originates from the Eritrea-Ethiopia Plateau. The GSIS is the breadbasket for the Eastern Region of Sudan with over half a million inhabitants. This research focused on sedimentation problem and its remedial measures at Fota diversion intake. The sediment deposition in front of Fota diversion intake reached up to 1.5 m depth. This deposition at the diversion intake plus sedimentation in the canal networks reduces the Fota block irrigable land by 75%. Therefore, providing remedial measures to the sedimentation problem at Fota intake would directly impact the livelihood of 100's of poor farmers. The sedimentation at the vicinity of the diversion intake was analysed using a Delft3D model. The model was calibrated and validated using observed water levels at Fota diversion intake, with a coefficient of determination (R2) of 85% and 72% respectively. The model result under existing condition showed a 1.6 m sediment deposition at the main intake which in fact is the real situation on the ground. Alternative, sediment remedial measures based on local knowledge of farmers and technicians were modelled. Sedimentation at the intake could be reduced to almost zero if additional three Spurs (100 m, 50 m and 120 m long) are constructed on the opposite bank of the diversion at 25 m, 100 m and 200 m upstream the diversion structure respectively, and increasing the intake sill level by 1 m.

Highlights

  • Spate irrigation is a type of water management that flood water from mountain catchments, laden with sediment concentration as much as 10%, is diverted from rivers and spread over large areas

  • The Gash River originates from the Eritrean-Ethiopian Plateau, and ends up in a Delta in Sudan, providing spate water for the Gash Spate Irrigation Scheme

  • Since there was no continuous sediment deposition data around Fota Diversion Intake for model calibration, qualitative calibration and total depth of sediment deposited on the sill of the intake was adopted

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Summary

Introduction

Spate irrigation is a type of water management that flood water from mountain catchments, laden with sediment concentration as much as 10%, is diverted from rivers and spread over large areas. Sedimentation is a real challenge for spate irrigation systems at the diversion structure from the river source. Flood water arrive with high sediment load, and creates serious problems at diversion intakes and canals network if it is not controlled and managed properly [3,4]. The major part of this sediment deposited in the GSIS, more noticeably at the canal and diversion intake structures. The sediment deposition in front of Fota diversion intake reaches up to 1.5 m. Providing remedies to the sedimentation problem at Fota intake would directly impact the livelihood of 100's of poor farmers who solely depends on agriculture.

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