首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Impacts of flow regulation on geomorphic adjustment and riparian vegetation succession along an anabranching reach of the Upper Yellow River
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Impacts of flow regulation on geomorphic adjustment and riparian vegetation succession along an anabranching reach of the Upper Yellow River

机译:流量调节对沿着黄河上游近地区的地貌调整和河岸植被连续的影响

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摘要

Closure of Longyangxia Dam in 1986, the uppermost large dam along the trunk stream of the Upper Yellow River in western China, permanently altered the flow regime in Guide reach, an anabranching section of river located 41 km downstream of the dam. Two smaller hydropower structures, Nina and Laxiwa Dams, were constructed between Longyangxia Dam and Guide in 2003 and 2009 respectively, but they had a minor influence on the flow regime. This study uses the Indicators of Hydrologic Alteration model, satellite imagery and field analyses to assess how the magnitude and duration of changes to the flow regime impacted upon geomorphic adjustments and riparian vegetation succession from 1987 to 2015. Flow impoundment resulted in near instantaneous reduction in the width of the active channel zone. Human activities have manipulated the additional floodplain areas created by these changes. Aggregation of mid-channel bars into larger compound features decreased channel multiplicity. Negligible bed incision likely reflects local supply of sediment from tributary sources downstream of the dam. Significant correlations are shown between changes to the balance between channel depositional and erosional processes induced by flow regulation and the functional composition of vegetation succession patterns. Maintenance of a higher water table for longer periods of time is inferred to have altered mutual interactions between hydrogeomorphic processes and riparian vegetation in this semi-arid setting.
机译:1986年关闭朗扬峡大坝,中国西部大黄河沿线的最高大坝,永久改变了导游的流动制度,河流在大坝下游41公里处的河流部分。两种较小的水电站,尼娜和距离龙阳峡谷和2009年和2009年的指导建造,但它们对流动制度的影响很小。本研究采用了水文改变模型,卫星图像和田间分析的指标,从1987年至2015年评估了对流动制度的幅度和持续时间对流动制度的影响程度和河岸植被连续。流量蓄水导致近瞬时减少活动通道区域的宽度。人类活动已操纵这些变化产生的额外洪泛区区域。中间通道杆聚集成较大的化合物特征,通道多重程度降低。可忽略不计的床切口可能反映了大坝下游支流源的局部沉积物供应。在流量调节诱导的信道沉积和侵蚀过程与植被连续模式的功能组成之间的平衡之间的变化之间显示了显着的相关性。在该半干旱设定中推断出更长的时间较长时间的较长时间的维持,以改变水力晶体过程和河流植被之间的相互相互作用。

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