Stochastic and analytical approaches for sediment accumulation in river reservoirs

Tanju Akar, Hafzullah Aksoy*

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

5 Citations (Scopus)

Abstract

Sediment accumulation in a river reservoir is studied by stochastic time series models and analytical approach. The first-order moving average process is found the best for the suspended sediment discharge time series of the Juniata River at Newport, Pennsylvania, USA. Synthetic suspended sediment discharges are first generated with the chosen model after which analytical expressions are derived for the expected value and variance of sediment accumulation in the reservoir. The expected value and variance of the volume of sediment accumulation in the reservoir are calculated from a thousand synthetic time series each 38 years long and compared to the analytical approach. Stochastic and analytical approaches perfectly trace the observation in terms of the expected value and variability. Therefore, it is concluded that the expected value and variance of sediment accumulation in a reservoir could be estimated by analytical expressions without the cost of synthetic data generation mechanisms.

Original languageEnglish
Pages (from-to)984-994
Number of pages11
JournalHydrological Sciences Journal
Volume65
Issue number6
DOIs
Publication statusPublished - 25 Apr 2020

Bibliographical note

Publisher Copyright:
© 2020, © 2020 IAHS.

Funding

The authors are grateful to the anonymous reviewers and Associate Editor, Dr Jesús Rodrigo-Comino, whose constructive comments improved the paper significantly. The authors thank also Asst. Prof. Halil Ibrahim Burgan, Istanbul Kultur University, and Ms Yonca Cavus, PhD candidate at Istanbul Technical University, for the figures.

FundersFunder number
T.C. İstanbul Kültür Üniversitesi
Istanbul Teknik Üniversitesi

    Keywords

    • Juniata River
    • moving average model
    • river reservoir
    • storage volume
    • suspended sediment discharge

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