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希腊莫诺斯湖/水库的可持续性评估。

Sustainability evaluation of Mornos Lake/Reservoir, Greece.

机构信息

Hellenic Centre for Marine Research, Institute of Oceanography, 46.7 km Athens-Sounio Avenue, 19013, Anavyssos, Attica, Greece.

Division of Raw Water Intake, Athens Water Supply and Sewerage Company SA, 16 Galatsiou Avenue, 11141, Athens, Attica, Greece.

出版信息

Environ Monit Assess. 2018 Jan 6;190(2):64. doi: 10.1007/s10661-017-6431-3.

Abstract

The modern climate trend and population growth have dramatically increased the need for maximization of the net benefit from the existing storage space in freshwater reservoirs. However, sedimentation in reservoirs through physical deposition and/or slope failures is a major threat to their productivity and life expectancy. In this context, the sedimentation impact on the sustainability of Mornos Lake/Reservoir, which is exceptionally vital for the ~ 3.1 million inhabitants of Athens, had to be evaluated. Therefore, a meticulous geophysical survey of the reservoir bed was conducted in 2015 for the very first time. Bathymetric, sidescan sonar, and seismic profiling datasets, all integrated with real-time kinematic (RTK) positioning, were analyzed for a realistic evaluation of the storage capacity loss. Approximately 18.2 × 10 m of lacustrine sediments derived through physical wedge-type deposition process and ~ 800,000 m of material produced by slope failures have covered the bottom since reservoir commissioning in 1981. This configures an average storage capacity loss of ~ 0.07% per year, which, however, is one of the lowest rates worldwide. Moreover, the 108-m-deep reservoir basin can presently accommodate a maximum active water volume of ~ 740 × 10 m. The siltation pattern and sediment transport pathways in the reservoir are principally controlled by vigorous turbidity underflows, which deliver sediment mainly to the dam area (deposition thickness up to ~ 7 m) as well as to the pumping area (deposition thickness up to ~ 4 m) posing there a future risk; nevertheless, according to the predicted lake bathymetry, this risk will be negligible till 2045.

摘要

现代气候趋势和人口增长极大地增加了从现有淡水库存空间中最大化净收益的需求。然而,水库中的淤积通过物理沉积和/或边坡失稳对其生产力和预期寿命构成了重大威胁。在这种情况下,必须评估莫尔诺斯湖/水库的淤积对可持续性的影响,该水库对雅典约 310 万居民的生活至关重要。因此,2015 年首次对水库床进行了细致的地球物理调查。对水深测量、侧扫声纳和地震剖面数据集进行了分析,并结合实时动态(RTK)定位,以对存储容量损失进行真实评估。自 1981 年水库投入使用以来,通过物理楔形沉积过程产生的约 18.2×10 m 的湖相沉积物和约 80 万 m 的边坡失稳物质已覆盖了底部。这构成了平均每年约 0.07%的存储容量损失,然而,这是全球最低的比率之一。此外,108 米深的水库盆地目前可容纳约 740×10 m 的最大可用水量。水库中的淤积模式和泥沙输移路径主要受强烈的浑浊底流控制,这些底流主要将泥沙输送到大坝区(沉积厚度高达约 7 m)和抽水区(沉积厚度高达约 4 m),从而构成未来的风险;然而,根据预测的湖床地形,这种风险到 2045 年将可忽略不计。

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