Recent morphological changes (2009-2022) on the floodplain of the Guadalporcún River, province of Cádiz (Southern Spain)

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In 2009 and 2013 two avulsion events occurred in the Guadalporcún River, a tributary of the Guadalete River, SW Spain. Google Earth and Geamap images acquired between 2002 and 2022 were examined and a timeline of events constructed. Exposed floodplain materials to a depth of up to 2 m reveal about 80 cm of sandy alluvium resting on a firm buried soil formed on older sandy alluvium with occasional pebble and boulder clasts. The avulsions, likely caused by logjams, breached the natural levee, and formed channels, less than 1 m deep in 2009 and more than 2 m deep in 2013. In 2013 the buried soil played an important role in the retreat of a knickpoint, the main process in avulsion channel formation. Following each avulsion event, a local landowner repaired the levee and levelled the floodplain, filling the avulsion channel with building rubble. The occurrence of two avulsion events separated by a few years shows that reestablishment of the original channel after the 2009 event was temporary and that similar events are likely to occur in the future.

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  • Research Article
  • Cite Count Icon 1
  • 10.4236/ojmh.2019.91002
Avulsion Dynamics in a River with Alternating Bedrock and Alluvial Reaches, Huron River, Northern Ohio (USA)
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  • Open Journal of Modern Hydrology
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The Huron River consists of alternating bedrock reaches and alluvial reaches. Analysis of historical aerial photography from 1950-2015 reveals six major channel avulsion events in the 8-km study area. These avulsions occurred in the alluvial reaches but were strongly influenced by the properties of the upstream bedrock reach (“inherited characteristics”). The bedrock reaches aligned with the azimuth of joint sets in the underlying bedrock. One inherited characteristic in the alluvial reach downstream is that the avulsion channels diverged only slightly from the orientation of the upstream bedrock channel (range 2 ° - 38 °, mean and standard deviation 12.1 ° ± 13.7 °). A second inherited characteristic is that avulsion channels were initiated from short distances downstream after exiting the upstream bedrock channel reach (range 62 - 266 m, mean and standard deviation 143.7 ± 71.0 m), which is a fraction of the meander wavelength (1.2 km). Field evidence shows that some avulsion channel sites were re-occupied episodically. In addition, two properties were necessary for channel avulsions: 1) avulsion events were triggered by channel-forming hydrologic events (5-year recurrence interval flows), but not every channel-forming hydrologic event resulted in an avulsion, and 2) channel sinuosity (P) increased to 1.72 - 1.77 prior to an avulsion then decreased to 1.65 - 1.70 following an avulsion, suggesting that P ≥ 1.72 is the “critical sinuosity” or triggering value for avulsions on the Huron River. In summary, for this river consisting of alternating bedrock and alluvial reaches, the bedrock reaches impose certain parameters on downstream alluvial reaches (including sediment supply, channel direction and avulsion channel position downstream after exiting a bedrock reach) while adjustments in sinuosity and sediment storage occur in the alluvial reaches.

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  • Cite Count Icon 4
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  • IEEE Robotics and Automation Letters
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