J. Windolf et al., MODELING OF SEASONAL-VARIATION IN NITROGEN-RETENTION AND IN-LAKE CONCENTRATION - A 4-YEAR MASS-BALANCE STUDY IN 16 SHALLOW DANISH LAKES, Biogeochemistry, 33(1), 1996, pp. 25-44
The mass balance for total nitrogen (N) was studied over a four-year p
eriod in 16 shallow mainly eutrophic Ist order Danish lakes. Water was
sampled in the main inlet of each lake 18-26 times annually, and from
the outlets and the lake 19 times annually. Water was also sampled fr
om minor inlets, although less frequently. N input and output were cal
culated using daily data on discharge (Q), the latter being obtained e
ither from the Q/H relationship based on automatic recordings of water
level (H) for the main in- and outlet, or by means of Q/Q relationshi
ps for the minor inlets. Annual mean N retention in the lakes ranged f
rom 47 to 234 mg N m(-2) d(-1), and was particularly high in lakes wit
h high N loading. Annual percentage retention (N-ret-y%) ranged from 1
1 to 72%. Non-linear regression analysis revealed that hydraulic reten
tion time and mean depth accounted for 75% of the variation in annual
mean N-ret-y% and, in combination with inlet N concentration, accounte
d for 84% of the variation in the in-lake N concentration. N-ret% vari
ed according to season, being higher in the second and third quarter t
han in the first and fourth quarter(median 18-19%). A simple model was
developed for predicting monthly nitrogen retention (N-ret-m) on the
basis of external N loading, the lake water pool of nitrogen N-pool, h
ydraulic loading and lake water temperature. Calibration of only two p
arameters on data from the randomly selected 8 out of 16 lakes rendere
d the model capable of accurately simulating seasonal dynamics of the
in-lake N concentration and N-ret-m in all 16 lakes. We conclude that
with regard to shallow, eutrophic lakes with a relatively low hydrauli
c retention time, it is now possible to determine not only annual mean
nitrogen retention, but also the seasonal variation in N-ret-m. Predi
ction of seasonal variation in N loading of downstream N-limited coast
al areas is thereby rendered much more reliable.