Meandering rivers form through fluid dynamics and sediment erosion-deposition processes
Geomorphological and fluid dynamic studies demonstrate that meandering river formation is driven by fluid flow instabilities and continuous sediment erosion and deposition processes along channel banks.
The claim addresses the established geomorphological mechanisms of meandering rivers, which are well-supported by numerous hydrodynamic and sediment transport models in the literature (e.g., papers 0, 1, 3, and 9). The papers detail bend stability, flow resonance, and erosion-deposition dynamics. There are no papers refuting this fundamental geomorphological principle.
Syunsuke Ikeda, Gary Parker, Kenji Sawai. Bend theory of river meanders. Part 1. Linear development. 1981. https://doi.org/10.1017/s0022112081000451
Analyzes the stability mechanisms of bend formation and channel sinuosity development in alluvial rivers.
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P. Blondeaux, G. Seminara. A unified bar–bend theory of river meanders. 1985. https://doi.org/10.1017/s0022112085002440
Develops a two-dimensional hydrodynamic and morphodynamic model showing how flow and boundary interactions initiate meanders.
ROSSELLA LUCHI, GUIDO ZOLEZZI, MARCO TUBINO. Bend theory of river meanders with spatial width variations. 2011. https://doi.org/10.1017/jfm.2011.200
Investigates the linear bend stability process and spatial variations that drive meander planform evolution.
Miao R, Howard AD, Dietrich WE. The sediment transport mechanics driving lateral accretion in muddy meanders.. 2025. https://doi.org/10.1073/pnas.2506462122
Models cohesive sediment transport, erosion, and deposition patterns (lateral accretion) that sustain meandering channels.
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