Fluxes of water and solute in a coastal wetland sediment. l. The contribution of regional groundwater discharge
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In situ experiment on groundwater control of the ecological zonation of salt marsh macrophytes in an estuarine area
2020, Journal of HydrologyCitation Excerpt :Different salt marsh macrophytes have different tolerances to salinity, so the ecological zonation of salt marsh macrophytes is significantly affected by soil salinity (Julkowska and Testerink, 2015; Xue et al., 2018)). Many studies have shown that these abiotic factors are related to the elevation and hydrological processes of salt marshes (Silvestri et al, 2005), especially in relation to groundwater processes in shallow soil (Gardner, 1973; Hemond and Fifield, 1982; Harvey et al., 1987; Harvey and Odum, 1990; Nuttle and Harvey, 1995). Groundwater process is the main route of solute migration in soil (Guo et al., 2008, 2011, 2013, 2014, 2016, 2019; Famiglietti, 2014).
Assessing the contribution of porewater discharge in carbon export and CO<inf>2</inf> evasion in a mangrove tidal creek (Can Gio, Vietnam)
2018, Journal of HydrologyCitation Excerpt :In a typical tidal creek, no direct freshwater input from upstream rivers/streams occurs. At a daily time scale, water outflow, evapotranspiration and intertidal storage account for losses in the water budget (Michot et al., 2011; Nuttle and Harvey, 1995; Speer et al., 1991). Mutual feedback processes between hydrodynamics and geomorphology define the natural system of tidal creeks.
Tidal marsh creation
2018, Coastal Wetlands: An Integrated Ecosystem ApproachHydrogeology and geochemistry of near-shore submarine groundwater discharge at Flamengo Bay, Ubatuba, Brazil
2008, Estuarine, Coastal and Shelf ScienceCitation Excerpt :While the intercomparison experiment examines SGD on a variety of scales, the work reported on here quantifies SGD on the small scale of a beach transect in the near-shore region where much of the discharge is expected to take place. Previous SGD studies (for example, Harvey and Odum, 1990; Vanek, 1993; Nuttle and Harvey, 1995; Staver and Brinsfield, 1996; Robinson, 1996) have been carried out on a small scale (tens to hundreds of meters), while previous SGD intercomparison experiments (Burnett et al., 2002; Burnett et al., 2006; Martin et al., 2007) have examined SGD on multiple scales, including the local scale. The granitic rocks of the study area are representative of the extensive Pre-Cambrian shield region of eastern Brazil.
Nitrogen Dynamics of Coastal Salt Marshes
2008, Nitrogen in the Marine Environment