Abstract
The paper presents an analysis of the morphological changes created on the Moldova River lower course. The studies and researches were carried out on the sector around Pildeşti locality, where Roman water catchment is located. The successive floods from 1994 to 2018 have morphologically modified the Moldova River minor river bed, which determined supply parameters of the wells located on the left bank of the river. The minor river bed moves horizontally during floods due to the degradation of the jetties and the enclosure beams. The floods of 2016 and 2018 partially and totally destroyed some of the riverbed's shore protections. Also, part of the shore protection works have been degraded, which has influenced the stability of the Moldova River left bank. The floods in the past ten years have led to the displacement of the minor river bed towards the right riverbank by breaking the old enclosure dikes and the jetties. Studies conducted during 2012-2018 analysed hydrological, hydraulic, morphological and topographic parameters on the considered river sector. The research analysed the concurrence of regulation and protection works in the water catchment area during floods. The flood of 2016 forced the restoration of the Moldova River minor river bed, to ensure the optimum wells operation.
Highlights
Significant climate changes have taken place over the last 30 years in Europe and, implicitly, in Romania
A set of research was conducted on the Moldova River study section between 2014 and 2018. They analysed the behaviour of river regulation and shore protection works during floods
The analysis of transit flows was performed over time periods of 10 years, 25 years and 55 years
Summary
Significant climate changes have taken place over the last 30 years in Europe and, implicitly, in Romania. These have generated a negative impact on the environment. Climate change has influenced the annual distribution of precipitation and flow in river basins. The seasonal change of meteorological parameters creates. The development and evolution of the maximum flows on rivers was influenced, causing flood waves with disaster effects. Changing hydrological parameters influence the morphological evolution of the river bed, and the behaviour of river bed and riparian area constructions (Ichim et al, 1989)
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