[Impact of macrofaunal activities on the DIN exchange at the sediment-water interface along the tidal flat of Yangtze River estuary].

Huan Jing Ke Xue

Key Laboratory of Geo-information Science of the Ministry of Education, College of Resources and Environment Science, East China Normal University, Shanghai 200062, China.

Published: November 2005

AI Article Synopsis

  • Macrof fauna, like the bivalve Corbicula fluminea, significantly influence pollutant exchange and nutrient cycling in sediment-water interfaces.
  • In short-term experiments, their burrowing increases the release of ammonium (NH4+) and nitrate (NO3-) from sediments into the water.
  • Over longer periods, these activities enhance nitrogen dynamics and organic matter breakdown, leading to greater NH4+ release into the overlying water.

Article Abstract

The macrofaunal activities exert intensive and extensive influences on the accumulation, transportation, exchange and geochemistry processes of pollutants and redox sensitive elements around the sediment-water interface. Based on the simulated and contrastive analysis method, effects of bivalve Corbicula fluminea activities on dissolved inorganic nitrogen (DIN) exchange between sediment-water interface in different experimental conditions and nitrogen biogeochemical cycling along the tidal flats of Yangtze River estuary are discussed. In short time experiment, Corbicula fluminea burrowing activities increased NH4+ release from sediments, and NO3- efflux to overlying water was much more in Corbicula fluminea inhabiting core. During long time incubation, NH4- and N released in turn from the sediments, bioturation can facilitate NH4- release from the sediments at the beginning of incubation, and stronger nmistrification derived from bioturbation witin the sediments enlarge Nsedim concentration. Disturbance and bioirrigation of Corbicula flumuminea can accelerate organic matter mineralization and N(DIN) exchange between overlying water and pore water, result in a larger release from NH4+ pool in top-sediment to overlying water. In conclusion, by means of excretion, burrowing, bioirrigation and biotuary ation, Corbicula fluuminea burrowing activities can evidently modify the nitrogen dynamics in sediment-water system.

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