Seasonal and long-term trends in the rate of calcium carbonate (CaCO3)
deposition are documented for Ca2+ polluted Onondaga Lake, New York.
These observations are based on particulate inorganic carbon and parti
culate calcium analyses of sediment trap collections, made weekly over
the May-September interval for 10 years. Continuous deposition of CaC
O3 was evident for the monitoring period of all 10 years. The average
rate of CaCO3 deposition for the deployment interval decreased from ab
out 0.196 to 0.082 mol . m(-2). d(-1) following the closure of the ind
ustrial source of Ca2+ pollution. This decline was generally consisten
t with the reductions in Ca2+ loading and lake Ca2+ concentrations ove
r the same period. The prevailing rate of CaCO3 deposition in Onondaga
Lake remains substantially higher than the rates documented for three
other hardwater lakes in the literature. Calcium carbonate is the pri
mary component and principal regulator of the dynamics of total solids
deposition in the lake. Copyright (C) 1996 Elsevier Science Ltd