Title of article :
Concentrations of suspended particulate organic
carbon in the tidal Yorkshire Ouse River and Humber
Estuary
Author/Authors :
R.J. UnclesU، نويسنده , , P.E. Frickers، نويسنده , , A.E. Easton، نويسنده , , M.L. Griffiths، نويسنده , , C. Harris، نويسنده , , R.J.M. Howland، نويسنده , , R.S. King، نويسنده , , A.W. Morris، نويسنده , , D.H. Plummer، نويسنده , , A.D. Tappin، نويسنده ,
Issue Information :
هفته نامه با شماره پیاپی سال 2000
Abstract :
Data are presented for particulate organic carbon POC. and particulate nitrogen PN. concentrations in the
Humber Estuary and tidal River Ouse Estuary. The POC data were derived from approximately monthly surveys and
are consistent with data reported for suspended particulate matter SPM. in the non-tidal River Ouse the freshwater
river. and with SPM, or bed sediments, in estuarine ecosystems such as the Mississippi, Delaware, San Francisco Bay,
Tolo Harbour, the Vellar Estuary and Cochin Backwater, as well as the Loire, Gironde, Ems and Tamar Estuaries.
Relative to the dry weight of SPM, the Humber-averaged organic carbon and nitrogen percentages during the year
February 1995]March 1996 were 2.6"0.6% mean and S.D.. and 0.21"0.04%, respectively. The ratio of Humberaveraged
POC to Humber-averaged PN was 13"3. Higher POC levels were observed near the Humber’s mouth and
in the adjacent coastal zone during ‘bloom’ conditions, and in the upper estuarine reaches during large, winter and
springtime freshwater inflows. At these times of high runoff, the POC content of SPM increased progressively
up-estuary from the coastal zone to the tidal River Ouse. When inflows became very low, during late spring to early
autumn of 1995, both the freshwater]saltwater interface FSI. and the strengthening turbidity maximum TM. moved
further up-estuary and the POC content of SPM in the upper reaches of the Ouse became lower compared with that
immediately down-estuary. This led to a poorly defined POC maximum near the confluence of the Humber, Ouse
and Trent, before POC eventually decreased again towards the coastal zone. The lower POC contents in the upper
estuarine reaches of the tidal Ouse may have been partly due to POC respiration by heterotrophic bacteria attached
to SPM within the TM, consistent with the severe oxygen depletion observed there during high turbidity, summertime
spring tides.
Keywords :
Yorkshire Ouse , Humber estuary , Particulate nitrogen , dissolved oxygen , Particulate organic carbon
Journal title :
Science of the Total Environment
Journal title :
Science of the Total Environment