Nm. Burns, USING HYPOLIMNETIC DISSOLVED-OXYGEN DEPLETION RATES FOR MONITORING LAKES, New Zealand Journal of Marine and Freshwater Research, 29(1), 1995, pp. 1-11
Volumetic hypolimnetic oxygen depletion, caused primarily by the decom
position of organic material in the hypolimnion (VHDR(org)), is consid
ered to be an important indicator of the trophic state of lakes and is
used to detect change of trophic state. The observed volumetric hypol
imnetic depletion rate (VHDR(obs)) is usually different from VHDR(org)
because of phenomena which can alter the concentrations of oxygen in
the hypolimnion. The nine different phenomena which can affect the rat
e at which the observed hypolimnetic dissolved oxygen depletes are rev
iewed. In many instances, if the limnology of the system is understood
, the perturbations to the hypolimnetic respiration rate, VHDR(org), c
aused by these phenomena can be ignored and VHDR(obs) used for lake ma
nagement. Guidance is provided as to when the effects of these phenome
na can be ignored and when they cannot be. Should corrections be neces
sary, methods for calculating the effects of physical perturbations ar
e outlined. However, most of the effects caused by biological perturba
tions from changes in algal species cannot be eliminated, except for t
hose caused by hypolimnetic production.