Modification of meander migration by bank failures

D. Motta, E. J. Langendoen, J. D. Abad, Marcelo Horacio Garcia

Research output: Contribution to journalArticle

Abstract

Meander migration and planform evolution depend on the resistance to erosion of the floodplain materials. To date, research to quantify meandering river adjustment has largely focused on resistance to erosion properties that vary horizontally. This paper evaluates the combined effect of horizontal and vertical floodplain material heterogeneity on meander migration by simulating fluvial erosion and cantilever and planar bank mass failure processes responsible for bank retreat. The impact of stream bank failures on meander migration is conceptualized in our RVR Meander model through a bank armoring factor associated with the dynamics of slump blocks produced by cantilever and planar failures. Simulation periods smaller than the time to cutoff are considered, such that all planform complexity is caused by bank erosion processes and floodplain heterogeneity and not by cutoff dynamics. Cantilever failure continuously affects meander migration, because it is primarily controlled by the fluvial erosion at the bank toe. Hence, it impacts migration rates and meander shapes through the horizontal and vertical distribution of erodibility of floodplain materials. Planar failures are more episodic. However, in floodplain areas characterized by less cohesive materials, they can affect meander evolution in a sustained way and produce preferential migration patterns. Model results show that besides the hydrodynamics, bed morphology and horizontal floodplain heterogeneity, floodplain stratigraphy can significantly affect meander evolution, both in terms of migration rates and planform shapes. Specifically, downstream meander migration can either increase or decrease with respect to the case of a homogeneous floodplain; lateral migration generally decreases as result of bank protection due to slump blocks; and the effect on bend skewness depends on the location and volumes of failed bank material caused by cantilever and planar failures along the bends, with possible achievement of downstream bend skewness under certain conditions. Key Points Cantilever failure impacts migration through horizontal/vertical floodplain material heterogeneity Planar failure in low-cohesion floodplain materials can affect meander evolution Stratigraphy of the floodplain materials can significantly affect meander evolution

Original languageEnglish (US)
Pages (from-to)1026-1042
Number of pages17
JournalJournal of Geophysical Research: Earth Surface
Volume119
Issue number5
DOIs
StatePublished - May 2014

Fingerprint

meanders
meander
floodplains
floodplain
Erosion
Planforms
erosion
planforms
Stratigraphy
skewness
stratigraphy
Bank protection
cut-off
horizontal distribution
bank erosion
erodibility
vertical distribution
material
cohesion
Hydrodynamics

Keywords

  • bank erosion
  • computer modeling
  • floodplain soil heterogeneity
  • meander migration
  • meander planform shape
  • slump block protection

ASJC Scopus subject areas

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Modification of meander migration by bank failures. / Motta, D.; Langendoen, E. J.; Abad, J. D.; Garcia, Marcelo Horacio.

In: Journal of Geophysical Research: Earth Surface, Vol. 119, No. 5, 05.2014, p. 1026-1042.

Research output: Contribution to journalArticle

Motta, D. ; Langendoen, E. J. ; Abad, J. D. ; Garcia, Marcelo Horacio. / Modification of meander migration by bank failures. In: Journal of Geophysical Research: Earth Surface. 2014 ; Vol. 119, No. 5. pp. 1026-1042.
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KW - meander planform shape

KW - slump block protection

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