Ar. Rendell et al., NUTRIENT CYCLING IN THE GREAT OUSE ESTUARY AND ITS IMPACT ON NUTRIENTFLUXES TO THE WASH, ENGLAND, Estuarine, coastal and shelf science, 45(5), 1997, pp. 653-668
A programme of surveys of the Great Ouse estuary (England) was conduct
ed to investigate the cycling of nutrients during mixing and to quanti
fy nutrient budgets for the estuary. The Great Ouse estuary is shallow
, well mixed and relatively turbid, and the dominant source of fresh w
ater to The Wash. Surveys were conducted once or twice a month between
February 1992 and January 1994 at high tide to yield seasonal and int
erannual information. High levels of chlorophyll a (>100 mu g l(-1)),
oxygen supersaturation (>120%) and non-conservative nutrient distribut
ions during spring and summer periods of low freshwater flow strongly
suggest that primary production in the low-salinity reaches of the est
uary may significantly modify nutrient fluxes to The Wash, despite the
relatively high turbidity. Zn support, calculated nutrient budgets in
dicate that biological removal in the river and estuary during the gro
wing season results in depleted nutrient fluxes and higher N:Si and P:
Si ratios which may affect primary production in coastal waters by con
tributing to the shift in species dominance from diatoms to flagellate
s and affecting the likelihood of bloom conditions occurring during th
e summer months. However, the influence of estuarine biological proces
ses on riverine nutrient fluxes is interrupted by periods of high fres
hwater flow, more characteristic of the winter months, which result in
high flushing rates. Under such conditions, nutrient distributions re
vert to a more conservatively mixed regime. This fundamental control e
xerted by freshwater flow generally limits the significance of estuari
ne processes on an annual basis, the exception being the inorganic rem
oval of phosphate in the low-salinity reaches of the estuary which acc
ounts for one-third of the annual input to the head of the salinity gr
adient. Given the character of this agriculturally impacted estuary, w
hich permits the relatively straightforward identification and quantif
ication of nutrient cycling processes, results from this study may hav
e wider application. (C) 1997 Academic Press Limited.