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Suspended sediment load at the lowermost Ebro River (Catalonia, Spain)

机译:最低的埃布罗河(西班牙加泰罗尼亚)悬浮泥沙负荷

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Several attempts to estimate the suspended load and the sediment deficit caused by the reservoirs have been carried out in the lower Ebro River. However, existing data are scarce, scattered along time and space, and obtained under different hydrological conditions and methods. This study estimate the presently suspended sediment load of the lowermost Ebro River, using field data collected during three consecutive years at different verticals of a cross-section and covering a large range of discharges. In addition, the daily suspended load for the last 30 years has been reconstructed and validated. The suspended load for the period 2007-2010 has been estimated at 84,000 t/y (+/- 9800 t) while 99,500 t/y (+/- 18,000 t) accounted for 1981-2010 period. Approximately, 80% of the total suspended load (period 2007-2010) has been transferred as inorganic load. A significant seasonal variability in the total (organic and inorganic) suspended load is observed. Therefore, two distinct cycling phases in the suspended load production and transfer has been inferred: an initial phase in which the sediment was prepared into the basin followed by a second phase in which most of the load was transferred downstream. These two phases are governed by the relative temporal location of the natural floods and the river regulation from the reservoirs. Nowadays, less than 1% of suspended load is transferred compared to pre-dams construction. The current levels of suspended load are very low and not enough to supply the material needed to maintain the delta elevation and avoid coastal retreat. The sustainability of the lower Ebro River and its delta could only be guaranteed by the implementation of a new reservoir management concept with the allocation of an appropriate liquid and solid flow regime. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:在埃布罗河下游进行了几次估算悬浮物和水库造成的泥沙淤积的尝试。但是,现有数据稀少,并沿时间和空间分散,并且是在不同的水文条件和方法下获得的。这项研究使用连续三年在横截面的不同垂直方向收集的,覆盖大范围排放物的连续三年的实地数据,估算了埃布罗河最下游目前的悬浮泥沙负荷。此外,最近30年的每日悬浮负荷已经过重建和验证。估计2007-2010年的悬浮负荷为84,000吨/年(+/- 9800吨),而99,500吨/年(+/- 18,000吨)占1981-2010年的时期。大约有80%的总悬挂负荷(2007-2010年)已作为无机负荷转移。在总(有机和无机)悬浮负荷中观察到明显的季节性变化。因此,推断出悬浮负荷产生和转移的两个不同的循环阶段:初始阶段,沉积物被制备到盆地中,然后是第二阶段,其中大部分负荷被转移到下游。这两个阶段受自然洪水的相对时间位置和水库的河流调节的支配。如今,与大坝前建设相比,仅转移了不到1%的悬浮负荷。当前的悬浮负荷水平非常低,不足以提供维持三角洲海拔和避免沿海退缩所需的材料。埃布罗河下游及其三角洲的可持续性只能通过实施新的水库管理概念并分配适当的液体和固体流态来保证。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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