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CHANNEL ADJUSTMENTS AND ISLAND DYNAMICS IN THE BRENTA RIVER (ITALY) OVER THE LAST 30 YEARS
Author(s) -
Moretto J.,
Rigon E.,
Mao L.,
Picco L.,
Delai F.,
Lenzi M. A.
Publication year - 2014
Publication title -
river research and applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.679
H-Index - 94
eISSN - 1535-1467
pISSN - 1535-1459
DOI - 10.1002/rra.2676
Subject(s) - floodplain , riparian zone , channel (broadcasting) , hydrology (agriculture) , river morphology , erosion , bank erosion , flood myth , tributary , woodland , geology , hydropower , vegetation (pathology) , natural (archaeology) , main river , physical geography , sediment , geography , geomorphology , ecology , archaeology , habitat , cartography , medicine , paleontology , geotechnical engineering , engineering , pathology , electrical engineering , biology
Many gravel bed rivers in the European Alpine area suffered different ranges and types of human pressure that modified their morphology and altered their processes. This work presents the case of the middle portion of the Brenta River, historically impacted by human activities such as floodplain occupations, bank protection, gravel mining, hydropower schemes and water diversion. Dam operation and gravel mining have produced considerable modifications in the natural sediment regime generating important morphological channel responses (narrowing and incision). Large areas of the former active channel have been colonized by riparian vegetation, both as islands and as marginal woodlands. Overall, the river changed its morphological pattern from braided to wandering. The present study analyses the timing and extent of the planform morphological changes that occurred over the last 30 years along the middle portion of the river (20 km long) through the examination of aerial photos, repeated topographic measurements and hydrological data. A series of recent aerial photos (1981, 1990, 1994, 1999, 2003, 2006, 2008, 2010 and 2011) have been used to assess the medium and short‐term morphological changes of the floodplains and the active channel area. As to the medium‐term modification, the recent changes in in‐channel gravel mining have determined a new trend of active channel widening through erosion of vegetated areas. The analysis has also allowed to assess the morphological effect of single flood events. Only floods with recurrence interval higher than 8–10 years appear to be able to determine substantial erosion of floodplain and island margins. Copyright © 2013 John Wiley & Sons, Ltd.