Advective flows rapidly transport water, solutes, and particles into and out of permeable
sand beds and significantly affects the biogeochemistry of coastal environments. In this …

The coastal zone of the Baltic Sea is diverse with strong regional differences in the physico-
chemical setting. This diversity is also reflected in the importance of different biogeochemical …

Meiobenthology is the science of the tiny animals that live in huge numbers in all aquatic
sediments. This fully revised and enlarged second edition emphasizes new discoveries and …

Nearshore (littoral) habitats of clear lakes with high water quality are increasingly
experiencing unexplained proliferations of filamentous algae that grow on submerged …

A carbon budget for the northwest European continental shelf seas (NWES) was
synthesized using available estimates for coastal, pelagic and benthic carbon stocks and …

Submarine groundwater discharge to coastal waters can be a significant source of both
contaminants and biologically limiting nutrients. Nitrogen cycling across steep gradients in …

The biogeochemical reactivity of sandy beach aquifers is closely linked to physical flow and
solute transport processes. Thus, a clearer understanding of the hydrodynamics in the …

Dissolution of marine sediment is a key source of dissolved iron (Fe) that regulates the
ocean carbon cycle. Currently, our prevailing understanding, encapsulated in ocean …

The effects of advective pore water exchange driven by shallow water waves on the oxygen
distribution in a permeable (k= 3.3 x 10− 12 to 4.9 x 10− 11 m2) natural sediment were …

Wave‐generated shear stresses are the main mechanism responsible for sediment erosion
on tidal flats and regulate both sediment concentrations in the water column and, together …