Sedimentation Analysis of Kabul River by Using Hec-ras

Raji, Baz Mohammad; Turabi, Hamidullah; Nasimi, Mohammad Nasim

doi:10.21203/rs.3.rs-2290973/v1

Cited by 1 publication

(1 citation statement)

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“…Sedimentation rates might differ signi cantly between reservoirs because of a variety of in uencing factors [ 18,19], including rainfall, erosion rates, catchment characteristics, and reservoir operation plans [ 20]. Furthermore, the sediment transport rates are impacted by climate change and human activity along the river [ 21].…”

Section: Introductionmentioning

confidence: 99%

Analyzing Sedimentation Patterns in the Naumure Multipurpose Project (NMP) Reservoir using 1D HEC- RAS Modeling

Dahal,

Kunwar,

Bhandari

et al. 2024

Preprint

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Naumure Multipurpose Project (NMP) featuring a 169 m high Concrete Face Rock Filled Dam (CFRD) is the proposed reservoir project in the West Rapti River with an installed capacity of 218.34 MW. Most of the rivers in Nepal carry significant sediment loads that will consequently catalyze reservoir sedimentation. This phenomenon prevails as the primary factor in reducing reservoirs useful life, making ineffective for both flood control and hydroelectricity generation. Ultimately, such process of sedimentation has adverse impacts on projects economic feasibility and long-term sustainability. Therefore, the objective of this research was to examine the expected sediment deposition pattern in the NMP reservoir throughout its operational period by employing 1D HEC-RAS model to simulate the sedimentation process. The model was simulated for 10, 20, 30, 40 and 50 years. Yang’s equation as a sediment transport function and Toffaleti as a fall velocity method were best suited for the river reach. The delta deposition was formed between 11 km to 22 km upstream of the dam region in the Jhimruk river, with the sediment deposition depth reaching peaks of about 23 m, 38 m, 39 m, 41 m and 49 m in 10, 20, 30, 40 and 50 years, respectively. Similarly, the delta deposition was formed between 13 km to 33 km upstream of dam region in the Madi river, with the sediment deposition depth reaching peaks of about 47 m, 62 m, 60 m, 68 m and 75 m in 10, 20, 30, 40 and 50 years respectively. Headcutting of delta deposition occurred between 20 to 30 year due to high flood during low stage of reservoir. Furthermore, the study revealed that about 6.22%, 11.61%, 15.94%, 22.96% and 25.65% of the storage capacity of NMP reservoir will be depleted in 10, 20, 30, 40 and 50 years respectively.

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Section: Introductionmentioning

confidence: 99%