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The role of reservoirs in global sediment budgets

机译:水库在全球沉积物预算中的作用

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摘要

Man-made reservoirs are an important sink for sediment eroded from the land and thus constitute an importantaspect of the sediment budget. Their impact has mostly been assessed at the scale of an individual river basin butrarely on a continental or even a global scale. Although there are recent estimates of global sediment retention bydams,these studies have solely focussed on the role reservoirs play in controlling sediment fluxes to the oceans, thuson their net impact for global sediment budgets. However, the net impact of reservoirs is much larger than thegross amount of sediment stored within all reservoirs on the globe. Furthermore, the impact of smaller waterholdingstructures is mostly neglected. In this paper, we present a first comprehensive assessment of global annualsediment storage within reservoirs based on sedimentation rates obtained from over 3700reservoirs, representing nearly 25% of the global storage capacity. We argue that at least 27 petagrams (Pg)sediment are stored annually in all larger reservoirs, with possible sediment retention of an additional 27 Pg insmaller man-made water bodies. These values are 2 to 4 times larger than the estimated sediment mass transportedannually to the global coastal ocean, and 8 to 15 times larger than the net reduction of sediment flux to the oceansattributed to reservoirs. These estimates provide minimum annual continental erosion rates and comparison withsoil erosion data suggest that soil erosion on agricultural land is not the dominant source of sediment deposited inreservoirs or exported to the ocean. In recent decades, reservoir sedimentation has become as least as importantas floodplain sediment storage and can nowadays be considered as one of the most important sediment sinks incontinental sediment budgets.
机译:人造水库是沉积物从陆地侵蚀的重要汇,因此构成沉积物预算的重要方面。它们的影响主要是在单个流域的规模上评估的,而在大陆乃至全球范围内却很少。尽管最近有关于全球沉积物滞留水坝的估计,但这些研究仅集中在水库在控制沉积物通向海洋的过程中所起的作用,从而对全球沉积物预算产生了净影响。但是,水库的净影响远远大于地球上所有水库内储存的沉积物的总量。此外,较小的持水结构的影响通常被忽略。在本文中,我们基于从3700多个水库中获得的沉积率(占全球存储量的近25%),对水库中全球年沉积物的存储量进行了首次综合评估。我们认为,在所有较大的水库中,每年至少存储27克沉淀物,在较小的人造水体中可能还会保留27 Pg的沉积物。这些值比每年输送到全球沿海海洋的估计沉积物质量大2至4倍,比分配给水库的海洋沉积物通量的净减少量大8至15倍。这些估算提供了最低的年度大陆侵蚀率,并且与土壤侵蚀数据的比较表明,农业土地上的土壤侵蚀不是沉积在水库中或出口到海洋的沉积物的主要来源。在最近几十年中,水库沉积已变得与洪泛区沉积物的储存一样不重要,如今已被视为洲际沉积物预算中最重要的沉积物汇。

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