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首页> 外文期刊>Journal of African Earth Sciences >Monitoring the lateral channel movements on the alluvial fan of Wadi Feiran drainage basin, South Sinai, Egypt using multi-temporal satellite imagery
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Monitoring the lateral channel movements on the alluvial fan of Wadi Feiran drainage basin, South Sinai, Egypt using multi-temporal satellite imagery

机译:使用多时相卫星图像监测埃及南西奈Wadi Feiran流域冲积扇的横向河道运动

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Human activities triggered various lateral channel movements over the alluvial fan of Wadi Feiran drainage basin, south Sinai, Egypt. Landsat TM images dated 1986, 1996, and 2001, along with a SPOT 4 XS image dated 2006 were acquired to monitor the lateral channel movement on the alluvial fan of Wadi Feiran through the last two decades. The lateral channel movements have been initiated by the channel avulsion of the incised channel of the alluvial fan as a result of obstructing the flow by developing a man-made barrier from the accumulated flood debris in the early years of 1990(s). The man-made barrier had evolved into an elevated concrete road of 3.75 m height with two culverts underneath directly south the fan apex by March 2007. These human activities enforced the incised channel to avulse in a new location leaving the original path and the active depositional lobe of the fan abandoned. Under the influence of successive flash flood events through the last twenty years, channel aggradations occurred resulting in channel braiding and channel widening processes in the reaches of the new formed distributary channels. The channel widening processes occurred on the expense of the inactive fan lobes located within and south the reaches of the new distributary channels. Observing the southward lateral growth of the reaches of the new formed distributary channels implies the possibility of forming a new active depositional lobe that could be merged with the abandoned depositional lobe of the fan.
机译:人类活动引发了埃及西奈南部Wadi Feiran流域冲积扇上方各种横向通道运动。采集了1986年,1996年和2001年的Landsat TM图像以及2006年的SPOT 4 XS图像,以监视过去20年中Wadi Feiran冲积扇横向通道的运动。横向通道运动是由冲积扇切开的通道的通道撕脱引起的,这是由于通过在1990年代初期从积聚的洪水残渣中形成人为屏障来阻碍流动而导致的。到2007年3月,人造屏障已发展成为一条高3.75 m的高架混凝土路,在扇形顶点正南下方有两个涵洞。这些人类活动迫使切开的河道在新的位置进行撕脱,从而保留了原始路径和活跃的沉积层。风扇的垂叶被抛弃。在过去二十年来连续的山洪暴发事件的影响下,河道发生了凝结,导致新形成的分流河道的河道编织和河道拓宽过程。通道拓宽过程的发生是以牺牲位于新分配通道内和南部的不活动风扇瓣为代价的。观察新形成的分流河道向南的横向增长,意味着有可能形成一个新的活动沉积叶,该沉积叶可以与风机的废弃沉积叶合并。

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