Social Science
Ali A. Lafta
Ali A. Lafta
Department of Marine Physics, Marine Science Center, University of Basrah,
The influence of Karun river inflow on salinity intrusion from the Arabian Gulf towards the upper reaches of the Shatt Al-Arab river estuary was evaluated by using Mike11, a one-dimensional numerical modeling technique. The simulations results indicated that, during the moderate and low flow conditions of the Shatt Al-Arab river, freshwater inflow from Karun river at 10 and 40 m3/s, respectively, could be capable of keeping salinity extent to not exceeded the confluence location of these two rivers. Additionally, the results indicated that in the case of a sharp decline of Karun river inflow, additional releasing of freshwater from the Tigris river can completely compensate for the Karun inflow. While in the case of cut off of Tigris river, the Karun inflow in the range of 60 m3/s could be able to keep salinity extent beyond the Abo Flous station during the simulation period. Furthermore, the possibility of discharging water with high levels of salinity from the farming projects located at the lower basin of Karun river towards the Shatt Al-Arab river estuary was taken into account. In such cases, the results suggested that during low and moderate flow conditions, freshwater inflow by about 250 and 225 m3/s, respectively, should be released from the Karun river to remains salinity extent below the Abo Flous location. A water management policy agreement between Iraq and Iran could be an effective solution to the salinity issue both in the Shatt Al-Arab river estuary as well as Karun river.
The study focuses on assessing the influence of the Karun River on salinity intrusion in the Shatt Al-Arab River estuary, located in the northwest of the Arabian Gulf. It uses numerical modeling to analyze how freshwater inflow from the Karun River affects salinity levels in the estuary.
Salinity intrusion is significant because it impacts water quality, ecosystems, and human activities such as agriculture, fishing, and drinking water supply. Understanding salinity dynamics is crucial for managing the estuary's resources and mitigating environmental challenges.
The Karun River influences salinity by providing freshwater inflow that dilutes seawater, reducing salinity levels in the estuary. The study examines how variations in the Karun River's flow affect the extent and intensity of salinity intrusion.
The study uses hydrodynamic and salinity transport models to simulate the flow and salinity dynamics in the Shatt Al-Arab estuary. These models incorporate data on river discharge, tidal forces, and bathymetry to predict salinity patterns.
The study finds that increased freshwater inflow from the Karun River significantly reduces salinity intrusion, while reduced inflow exacerbates it. Seasonal variations in river flow and tidal forces also play a critical role in shaping salinity patterns.
Tidal forces drive the mixing of freshwater and seawater, influencing the extent of salinity intrusion. The study highlights how tidal cycles interact with river flow to create complex salinity gradients in the estuary.
Reduced Karun River flow leads to increased salinity intrusion, which can harm ecosystems, reduce agricultural productivity, and affect drinking water quality. The study underscores the importance of maintaining adequate freshwater inflow to the estuary.
The study provides valuable insights into the relationship between river flow and salinity intrusion, supporting evidence-based water resource management. It highlights the need for policies that balance freshwater allocation and environmental sustainability.
Salinity intrusion can lead to the degradation of aquatic habitats, loss of biodiversity, and changes in species composition. It also affects vegetation and soil quality in surrounding areas, impacting agriculture and local livelihoods.
The study considers how changes in river flow patterns, potentially driven by climate change, could influence salinity intrusion. It emphasizes the need for adaptive management strategies to address future uncertainties in water availability.
Bathymetry, or the shape and depth of the estuary, influences water circulation and salinity distribution. The study uses detailed bathymetric data to improve the accuracy of its numerical models and predictions.
The findings can be applied to other estuaries facing similar challenges of salinity intrusion and freshwater inflow management. The numerical methods and insights from this study can inform sustainable water management practices globally.
Limitations include uncertainties in model inputs, such as river discharge data and future climate scenarios. The study also acknowledges the need for more detailed field measurements to validate and refine the models.
The study recommends maintaining sufficient freshwater inflow from the Karun River, implementing water conservation measures, and developing integrated water resource management plans to mitigate salinity intrusion and its impacts.
The main objective of the study is to numerically assess the influence of the Karun River's freshwater inflow on salinity intrusion in the Shatt Al-Arab River estuary. It aims to understand how variations in river flow affect salinity distribution and to provide insights for managing water resources in the region.
The Shatt Al-Arab River estuary is a vital waterway in the northwest Arabian Gulf, supporting agriculture, fisheries, and drinking water supply for millions of people. It is also ecologically significant, hosting diverse ecosystems that are sensitive to changes in salinity.
The Karun River, as a major tributary, provides freshwater inflow that counteracts seawater intrusion. The study shows that higher freshwater discharge from the Karun River reduces salinity levels, while lower discharge allows seawater to penetrate further upstream.
The study uses the **Environmental Fluid Dynamics Code (EFDC)**, a 3D hydrodynamic model, to simulate flow dynamics and salinity transport in the estuary. The model incorporates data on river discharge, tides, and bathymetry to predict salinity patterns under different scenarios.
The study finds that:
Tidal activity drives the mixing of freshwater and seawater, creating dynamic salinity gradients. The study highlights that tidal forces are particularly influential during low river flow conditions, exacerbating salinity intrusion.
Reduced Karun River flow leads to increased salinity intrusion, which can:
The study considers potential climate change impacts, such as reduced river flow due to droughts or upstream water diversions. It emphasizes the need for adaptive water management strategies to mitigate future salinity intrusion risks.
Bathymetry (the shape and depth of the estuary) influences water circulation and salinity distribution. The study uses detailed bathymetric data to improve the accuracy of its numerical simulations and predictions.
Salinity intrusion can:
The findings can inform water resource management by:
Limitations include:
The study recommends:
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2025 February | 8 | 8 |
2025 January | 78 | 78 |
2024 December | 66 | 66 |
2024 November | 80 | 80 |
2024 October | 81 | 81 |
2024 September | 73 | 73 |
2024 August | 55 | 55 |
2024 July | 61 | 61 |
2024 June | 50 | 50 |
2024 May | 69 | 69 |
2024 April | 74 | 74 |
2024 March | 75 | 75 |
2024 February | 50 | 50 |
2024 January | 48 | 48 |
2023 December | 43 | 43 |
2023 November | 58 | 58 |
2023 October | 35 | 35 |
2023 September | 26 | 26 |
2023 August | 21 | 21 |
2023 July | 40 | 40 |
2023 June | 26 | 26 |
2023 May | 38 | 38 |
2023 April | 47 | 47 |
2023 March | 48 | 48 |
2023 February | 1 | 1 |
2023 January | 5 | 5 |
2022 December | 28 | 28 |
2022 November | 62 | 62 |
2022 October | 32 | 32 |
2022 September | 31 | 31 |
2022 August | 55 | 55 |
2022 July | 50 | 50 |
2022 June | 94 | 94 |
2022 May | 46 | 46 |
Total | 1654 | 1654 |
Show by month | Manuscript | Video Summary |
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2025 February | 8 | 8 |
2025 January | 78 | 78 |
2024 December | 66 | 66 |
2024 November | 80 | 80 |
2024 October | 81 | 81 |
2024 September | 73 | 73 |
2024 August | 55 | 55 |
2024 July | 61 | 61 |
2024 June | 50 | 50 |
2024 May | 69 | 69 |
2024 April | 74 | 74 |
2024 March | 75 | 75 |
2024 February | 50 | 50 |
2024 January | 48 | 48 |
2023 December | 43 | 43 |
2023 November | 58 | 58 |
2023 October | 35 | 35 |
2023 September | 26 | 26 |
2023 August | 21 | 21 |
2023 July | 40 | 40 |
2023 June | 26 | 26 |
2023 May | 38 | 38 |
2023 April | 47 | 47 |
2023 March | 48 | 48 |
2023 February | 1 | 1 |
2023 January | 5 | 5 |
2022 December | 28 | 28 |
2022 November | 62 | 62 |
2022 October | 32 | 32 |
2022 September | 31 | 31 |
2022 August | 55 | 55 |
2022 July | 50 | 50 |
2022 June | 94 | 94 |
2022 May | 46 | 46 |
Total | 1654 | 1654 |