Radon (222 Rn) is a colourless, odourless, inert, and radioactive noble gas (t 1/2= 3.8 days)
that emanates from rocks and soils as a result of the alpha decay of its parent, radium (226 …

The number of studies concerning Submarine Groundwater Discharge (SGD) grew quickly
as we entered the twenty-first century. Many hydrological and oceanographic processes that …

The exchange of groundwater between land and sea is a major component of the
hydrological cycle. This exchange, called submarine groundwater discharge (SGD), is …

Both terrestrial and marine forces drive underground fluid flows in the coastal zone.
Hydraulic gradients on land result in groundwater seepage near shore and may contribute …

Mixing between meteoric water and sea water produces brackish to saline water in many
coastal aquifers. In this mixing zone, chemical reactions of the salty water with aquifer solids …

Submarine groundwater discharge (SGD) is now recognized as an important pathway
between land and sea. As such, this flow may contribute to the biogeochemical and other …

Nutrient input through submarine groundwater discharge (SGD) rivals river inputs in certain
regions and may play a significant role in nutrient cycling and primary productivity in the …

Coastal hydrogeologists and oceanographers now recognize the potentially significant
contribution that submarine groundwater discharge (SGD) could make to the coastal ocean …

The naturally occurring isotope radon-222 (222 Rn) is widely employed as a tracer for
groundwater discharge to lakes, lagoons, rivers, estuaries, and coastal oceans. Owing to the …

We hypothesize that nutrient cycling in a Gulf of Mexico subterranean estuary (STE) is fueled
by oxygen and labile organic matter supplied by tidal pumping of seawater into the coastal …