H. Cyr, EFFECTS OF WAVE DISTURBANCE AND SUBSTRATE SLOPE ON SEDIMENT CHARACTERISTICS IN THE LITTORAL-ZONE OF SMALL LAKES, Canadian journal of fisheries and aquatic sciences, 55(4), 1998, pp. 967-976
Sediment characteristics in the littoral zone of lakes affect the dist
ribution, biomass, and productivity of benthic organisms and affect ch
emical exchanges with the water column, yet we know very little about
their distribution. I tested whether sediment water and organic matter
content were related to site exposure and to basin morphology by comp
aring sediments along 12 transects in three small lakes (area <150 ha)
. The distribution of sediment water content in small lakes differed f
rom the general patterns described for large lakes and ocean. Sediment
water content was generally high in shallow waters (<2-5 m), decrease
d sharply to 30-50% within 20 m from shore, and increased again in the
deeper portion of the littoral zone. Fine sediments were retained in
the shallow littoral zone (<1.5 m) at sites with mean fetch <150 m. Th
e maximum depth at which sediments were mixed increased with increasin
g depth of the wave-mixed layer and with increasing slope of the subst
rate. The organic matter content (OM) of littoral sediments was closel
y related to their water content (WC) (log(OM) = -4.7 + 3.0 log(WC), r
(2) = 0.77, P < 0.001), and sediment organic content was very similar
in the upper and lower portions of the littoral zone.