2020年洪水对伊朗东南部萨迪吉河形态变化的影响

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Naimeh Rahimi , Somaiyeh Khaleghi , Alireza Salehipour Milani
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引用次数: 0

摘要

阿曼海沿岸平原每年都会发生洪水。2020年1月11日的洪水是贾斯克水文站记录的最高流量,导致伊朗萨迪吉河和洪泛平原发生变化。本研究的目的是探讨这次洪水事件对萨迪河下游的影响。这是第一次就洪水对阿曼海伊朗海岸短暂河流形态的影响进行研究。为此,根据河道形态将河道划分为A、B、C、D四段。通过对比本次洪涝前后的Sentinel-2卫星影像,分析了洪涝前后河流的形态计量参数、中心角、曲率系数、河网变化指数以及格局和水流功率。利用SMADA和HEC-RAS软件对不同汛期进行了洪水区划。结果表明:洪前河段平均中心角为85.61°,洪后河段平均曲率系数为77.72°,洪后河段平均曲率系数为1.22°;河网变化指数表明,A河段(2.35)、B河段(1.27)和C河段(0.39)以侵蚀为主,D河段(- 0.08)以沉积为主。本次洪水洪水功率较大,使B河段部分曲流与主河道分离。此外,这一百年一遇的洪水覆盖了12882.4 ha的面积,在规划和河流管理中应该考虑到这一点。因此,本研究为研究半干旱短命河流的洪水形态变化和洪水分区提供了新的思路,可用于未来的发展规划和河流修复。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effect of flood 2020 on the morphological changes of the Sadij River, Southeastern of Iran
River floods occur in the coastal plain of the Oman Sea every year. The flood on January 11, 2020 had the highest discharge recorded in the Jask hydrometric station that caused changes in Sadij River and floodplain in Iran. The aim of this research is to investigate the effect of this flood event on the lower part of the Sadij River. This is the first study has been conducted in relation to the impact of flooding on an ephemeral river morphology in the Iranian Coast of the Oman Sea. In this regard, the river channel was divided into four reaches (A, B, C, and D) based on the channel morphology. Then, the morphometric parameters of the river, central angle, curvature coefficient, River Network Change Index, as well as the pattern and the stream power were examined by comparing the Sentinel-2 satellite images before and after this flood. Also, the flood zoning was carried out using SMADA and HEC-RAS software in different flood return periods. The results showed that the average central angle and the average curvature coefficient were 85.61 and 1.42° for the four reaches before the flood and 77.72 and 1.22° for the post-flood period, respectively. Further, based on the River Network Change Index, the erosion was dominant process in the reaches A (2.35), B (1.27) and C (0.39) while deposition prevailed in the reach D (−0.08). The flood power of this flood was high and separating some of the meanders in reach B from the main river channel. Also, this flood with a return period of 100 years covers an area of 12,882.4 ha, which should be considered in planning and river management. Therefore, this study provides new insights into flood-induced morphological changes as well as flood zoning in semiarid ephemeral rivers that can be used for the future development plans and river restoration.
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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