Dp. Morris et Br. Hargreaves, THE ROLE OF PHOTOCHEMICAL DEGRADATION OF DISSOLVED ORGANIC-CARBON IN REGULATING THE UV TRANSPARENCY OF 3 LAKES ON THE POCONO PLATEAU, Limnology and oceanography, 42(2), 1997, pp. 239-249
The role of photochemical degradation of dissolved organic carbon (DOG
) on UV transparency (280-300 nm) was investigated in three Pocono Pla
teau lakes. Diffuse attenuation coefficients (K-dUV) in the epilimnia
of these lakes varied seasonally (39-81% decline from maximum Kd(320nm
)), with minimum K-dUV values occurring near summer solstice. Declines
in K-dUV corresponded to reductions in UV absorbance by dissolved mat
erial (a(dUV)), caused by declines in both DOC concentration and UV ab
sorptivity (a(d):[DOC]). The seasonal decline in K-dUV was also accomp
anied by substantial increases in an absorption coefficient ratio (a(d
250nm): a(d365nm)) and decreases in spectral slopes (S). Experimental
studies of photochemical degradation were also performed using filtere
d lake water and natural sunlight. Exposure to solar radiation produce
d a number of changes in optical parameters and DOC that resembled tho
se observed in the water column: a(dUV) (-35 to -52%), UV absorptivity
(-31 to -48%), a(d250nm):a(d365nm) (0 to + 39%), spectral slope, S (0
to 27%), and DOC concentration 0 to 20%). Changes in a(dUV) were corr
elated with absorbed UV dose. The derived rate constants were used in
a model to estimate the contribution of photochemical degradation of D
OC to water column declines in K-dUV. Results suggest that rates of ph
otochemical degradation were sufficient to account for the summer redu
ctions in K-dUV. Results suggest that rates of photochemical degradati
on were sufficient to account for the summer reductions in K-dUV obser
ved in the three lakes.