Sunlight Induced Photochemistry: Formation of Reactive Species
Project Number: R/PS-004, Completion Report
Start Date: 9/1/1989
Completion Date: 8/31/1991
Revision Date: 3/8/2012
|Principal Investigator(s)||1.||William J. Cooper, Drinking Water Res. Cen. FL International University*|
|This shows the current affiliation and may not match affiliation at time of participation. *|
|Source: Ohio Sea Grant College Program|
|Source Fund||State Match||Pass Through|
|Total||$ 29,091.00||$ 104,476.00||$ 0.00|
To assess the role of superoxide, O2-, the precursor of H2O2, in the fate and transport of organic pollutants in Lake Erie.
To determine the steady state concentrations of singlet oxygen, 1O2, in Lake Erie.
To assess the relative importance of these two photochemically produced reactive species in the fate and transport of organic pollutants in Lake Erie.
To assess the potential of using H2O2 as a chemical tracer for physical (mixing) processes.
1990: A project involving both laboratory and field studies has been proposed, the field studies involve the three major basins of Lake Erie, and are being conducted on the CSS LIMNOS. Methodology to examine the photochemical formation of H2O2 at various depths in at least one basin and to determine the major processes involved in the decomposition of H2O2 is being used. Experiments with selected pollutants will also be conducted, in the presence and absence of natural humic substances from Lake Erie.
Benefits & Accomplishments
We have described the spatial and temporal variability of H2O2 in the three basins of Lake Erie. This study will be extended to determine areal ???diel variability in Summer 1990.RESULTS: We have described the areal distribution of H2O2 in the three basins of Lake Erie. From these calculations, we have concluded that the total amount of H2O2 that is formed is very similar in all areas and that mixing plays a major role in determining the distribution of H2O2 in the water column.
We have determined the noon-time steady state concentrations of singlet oxygen in several lakes including Lake Erie Station 23 (Eastern Basin) and Station 357 (Western Basin). Singlet oxygen quantum yields at different wavelengths are also being determined for one Lake Erie water (Station 23). Singlet oxygen may be important in the fate and transport of organic pollutants in the lake.
The results to date are the first to be published on any major lake.
Publications & Media
|Cooper, William J., C. Shao, D.R.S. Lean, A.S. Gordon and F.E. Scully, Jr. 1994, Factors affecting the distribution of H2O2 in surface waters|
Environmental Chemistry of Lakes and Resevoirs, Lawrence A. Baker Editor. Made available by Ohio Sea Grant as OHSU-RS-396.
|Shao, C. 1992, Sunlight induced singlet oxygen formation in natural waters|
Made available on loan basis by Ohio Sea Grant (via National Sea Grant Depository) as OHSU-TD-053.