Pg. Eriksson, Interaction effects of flow velocity and oxygen metabolism on nitrification and denitrification in biofilms on submersed macrophytes, BIOGEOCHEMI, 55(1), 2001, pp. 29-44
Effects of water flow velocity on nitrification, denitrification, and the m
etabolism of dissolved oxygen and inorganic carbon in macrophyte-epiphyton
complexes were investigated in the present study. The metabolic rates were
measured in microcosms containing shoots of Potamogeton pectinatus L. with
epiphytic biofilms in the light and dark with no flow or with the flow velo
cities of 0.03 and 9 cm s(-1). Photosynthesis and respiration increased wit
h increasing water flow velocity. Rates of oxygen respiration were positive
ly correlated to the oxygen concentration of the water. Nitrification was n
ot significantly affected by flow velocity, but nitrification was higher in
light than in dark at 0.03 cm s(-1), but not at 9 cm s(-1). Denitrificatio
n was higher in stagnant water and at 9 cm s(-1) than at 0.03 cm s(-1) in t
he absence of oxygen, possibly due to complex effects of water flow velocit
y on the supply of organic matter to the denitrifying bacteria. Denitrifica
tion was always inhibited in light, and negatively correlated to the oxygen
concentration in dark. Epiphytic denitrification occurred only at low oxyg
en concentrations in flowing water, whereas in stagnant water, denitrificat
ion was present in almost oxygen saturated water. Therefore, because there
are little of water movements and high oxygen consumption in dense stands o
f submersed macrophytes, significant rates of epiphytic denitrification can
probably be found within submersed vegetation despite high oxygen concentr
ations in the surrounding water. In conclusion, this study shows that the w
ater flow and oxygen metabolism within submersed vegetation have minor effe
cts on nitrification, but significantly affect denitrification in biofilms
on submersed macrophytes.