Feedback of erosional-depositional processes generating anabranching patterns in a mega-river: the case of the Paraná River, Argentina.

LATRUBESSE, EDGARDO; PEREYRA, SOLEDAD; RAMONELL, CARLOS; SZUPIANY, RICARDO N.

San Francisco, California

Encuentro; AGU Fall Meeting; 2011

American Geophysical Union

A new category of "very large" rivers was recently proposed and defined as mega-rivers, which are those rivers with a Qmean of more than ~17,000m3/s. This category includes the nine largest rivers on Earth (Latrubesse, 2008) and the Parana River is one of the selected members of that peculiar group. The planform adjustment of mega-rivers is a variety of anabranching patterns characterized by the existence of alluvial islands. The processes and mechanisms involved in the generation of the different anabranching styles, however, are not well understood. The Paraná channel pattern has been classified as a low to moderate anabranching, low sinuosity with tendency to braided (Latrubesse, 2008) and having a meandering thalweg (Ramonell et al, 2002). We analyzed a reach of the middle Paraná in Argentina applying a combined multitemporal, hydraulic, sedimentologic and geomorphologic approach. Multitemporal geomorphologic maps, sedimentary descriptions of bars, islands and banks, volumetric calculations using multitemporal bathymetric charts, measurements with ADCP and bathymetric surveys with echosound, sediment transport estimations and the hydrological analysis of available data from gauge stations were some of the tools used in our research. The evolution of the reach was studied since 1908 to present. The reach is subdivided in two sub-reaches (named Chapeton and Curtiembre) which are comprised between nodal points. Chapeton has been in a more mature quasi-equilibrium state through the XX Century but the main channel in Curtiembre evolved from a single pattern to anabranching pattern since 1950s. We conclude that the generation of the anabranching pattern in the studied reach depends of a combination of factors such as the architecture of the floodplain and islands, the main role played by the morphodynamics and shifting of the thalweg, the availability of sediments (mainly bedload), the bedload transport capacity, bedforms architecture and the temporal variability of the effective discharge among other secondary factors. A feedback system coupling erosional/depositional processes at the decadal scale seems to be the main responsible for the generation of the complex anabranching pattern in such subreaches.