Fulvio Boano

TL;DR: In this paper, a review summarizes results from modeling studies and field observations about flow and transport processes in the hyporheic zone and describes the theories proposed in hydrology and fluid dynamics developed to quantitatively model and predict the hypheic transport of water, heat, and dissolved and suspended compounds from sediment grain scale up to watershed scale.

TL;DR: In this article, the authors present a special issue on groundwater-surface water (SW) interactions, which addresses the linkages between hydrology, biogeochemistry and ecology at nested scales and specifically accounts for small-scale spatial and temporal patterns of SW exchange.

TL;DR: In this article, the authors investigate the interplay of hydrological and biogeochemical processes in a duned streambed and their effect on spatial distribution of solutes, and employ a numerical model to simulate the turbulent water flow and the pressure distribution over the dunes, and then evaluate the flow field and the bio-geochemical reactions in the hyporheic sediments.

TL;DR: Boano et al. as mentioned in this paper used a physically-based morphodynamic model to predict the characteristics of the flow field in a meandering river and the temporal evolution of its planimetry.

TL;DR: In this paper, a model for the study of hyporheic exchange during unsteady conditions has been developed, which provides a sound analytical framework for the analysis of the effects of a varying stream discharge on the exchange between a stream and the hypheic zone.