4.7 Article

Analysing hydrological and sediment transport regime in two Mediterranean intermittent rivers

Journal

CATENA
Volume 196, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.catena.2020.104865

Keywords

Mediterranean catchments; Intermittent rivers; Hydrological regime; Suspended sediment transport

Funding

  1. Spanish Ministry of Science, Innovation and Universities [CGL2017-88200-R]
  2. Apulia Basin Authority
  3. Ministry of Innovation, Research and Tourism of the Autonomous Government of the Balearic Islands [FPI/2048/2017, MOB_017]
  4. COST Action [CA15113]
  5. Spanish Ministry of Education and Culture [FPU15/05239]

Ask authors/readers for more resources

Flow and sediment play vital roles in water quality and nutrient delivery in river systems. This study investigated the impact of various factors on flow regime and suspended sediment transport in two Mediterranean intermittent rivers, highlighting the influence of geology and rainfall variability.
Flow and the sediment regime affect water quality and nutrient delivery in all river systems and are fundamental in sustaining the river ecosystem. This study aims to identify the most relevant factors affecting the flow regime and the suspended sediment transport in two Mediterranean intermittent rivers: the Btiger (Spain) and the Carapelle (Italy). A set of hydrological indicators were used to characterize and classify the flow regime. High-resolution data, streamflow and suspended sediment concentration were used to quantify runoff and sediment yields at different temporal scales (annual, monthly, event). Rainfall, streamflow and sediment variables were used at the event scale to assess the rainfall-runoff-suspended sediment relationship through the Pearson correlation matrix. Hysteresis analysis provided information on sediment source dynamics. In the Btiger River, the high degree of flow intermittence was mainly due to the presence of carbonate lithology and forest land use at headwaters promoting low values of runoff coefficient (2-10%) and specific suspended sediment yield (SSY; 0.5-46 t km(-2) y(-1)). In the Carapelle River, the high values of annual runoff coefficient (14-35%), together with low flow intermittence and SSY (89-745 t km(-2)y(-1)) were related to clay and flyschoid lithology. Most of the annual sediment yield (SY, t) was transported during floods. In Btiger, SSY and maximum suspended sediment concentration (SSC(max )g l(-1)) were checked against runoff, peak discharge and antecedent rainfall. In Carapelle, SSY and SSC(max )were checked against the amount and intensity of rainfall. The catchment size and the spatial distribution of rainfall, land uses and lithology played important roles in the flow regime, suspended sediment transport and hysteretic behaviour. Characterization of the flow regime linked to its main physical drivers improved understanding of the hydrological response and sediment transport variability of intermittent rivers. This study provided valuable insights into water resource management, improving the prediction of spatial patterns and of the intensity of sediment transport in river basins.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available