Impacto de la represa de Gallito Ciego en la estabilidad de línea de costa en la desembocadura del río Jequetepeque, Perú

C. T. Correa, G. Ramírez
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引用次数: 1

Abstract

River plays an essential function in providing sediments to the beach stability but this importance has not yet been properly estimated on the Peruvian coastline. So, the aim of this study focuses on the role of river sediments in the stability of the coastline at the Jequetepeque river mouth, located at the northern coast of Peru. This river, whose basin covers an area of ​​4,200 square kilometers, provides in average more than 900 million cubic meters a year (MMC yr -1 ) of water, and 2.9-8.0 MMC yr -1 of sediments to the ocean. Since the start of the Gallito Ciego dam in 1987, more than 104 MMC of sediments were retained into the reservoir. In order to assess the impact of the dam on the stability of the river mouth, a comparison among different coastline moments (for the years 1962, 1980, 2003 and 2011) with the support of GIS, were made. The results showed that the river mouth retreat to the land between 2003 and 2011 with rates of -2.6 m year -1 . Moreover, the retreat of the coastline observed throughout the study area between 1962 and 2011, it could be related to the potential sea level rise and the trend of the worldwide beach erosion.
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galito Ciego大坝对秘鲁Jequetepeque河口海岸线稳定性的影响
河流在为海滩稳定提供沉积物方面起着重要作用,但秘鲁海岸线的这种重要性尚未得到适当的估计。因此,本研究的目的集中在河流沉积物在位于秘鲁北部海岸的杰克特佩克河口的海岸线稳定性中的作用。这条河的流域面积为4200平方公里,平均每年提供超过9亿立方米(MMC -1)的水,向海洋提供2.9-8.0 MMC -1的沉积物。自1987年Gallito Ciego大坝开始以来,超过104 MMC的沉积物被保留在水库中。为了评估大坝对河口稳定性的影响,在GIS的支持下,对不同年份(1962年、1980年、2003年和2011年)的海岸线力矩进行了比较。结果表明:2003 ~ 2011年,河口向陆地退缩的速度为-2.6 m /年。此外,在1962 - 2011年期间,整个研究区观测到的海岸线退缩可能与潜在的海平面上升和全球海滩侵蚀趋势有关。
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