The Effect of UV-B Radiation on Dissolved Organic Matter and Nitrogen Biogeochemistry in Aquatic Environments
Abstract
Peatlands are globally important reservoirs of carbon and represent important freshwater catchments in many regions. These waters generally contain high levels of dissolved organic matter (DOM), which contains a significant fraction of chromophoric, dissolved organic material (CDOM). CDOM is primarily responsible for light attenuation in these waters and affects a variety of biogeochemically relevant photo-processes including the formation of climatically active trace gases such as CO2, CO, COS and the release of essential plant micro-nutrients such as ammonium. Significant increases in DOM concentrations have been observed in various peatland waters over recent years, associated with increases in temperatures linked to global climate change. UV-B fluxes have also been projected to increase in the future as a consequence of stratospheric ozone depletion. Enhanced UV-B radiation can affect the balance between the biological processes that produce DOM and the chemical and microbial processes that degrade it. This infers that the rate of photochemical release of nutrients such as ammonium (photo-ammonification) is also likely to increase with increasing incident UV-B radiation. Samples of freshwater, riverine and marine, filtered (0.2 ìM) water were exposed to short-term natural and solar simulated irradiation which reduced their absorbance at 350 nm (a350) and total fluorescence intensity within the UV and visible regions and also produced changes in fluorescence excitation-emission matrix (EEM) measurements, such as the hypsochromic shift of peak A towards shorter wavelengths. Samples were taken from a variety of aqueous environments predominantly from Northern Scotland peatland freshwater catchments but also from the River Tyne, North East England and from the Iberian Coast, Atlantic Ocean, covering the a350 range 0.3 to 50 m-1. The photo-chemical release of ammonium from aquatic dissolved organic matter (DOM) was also concurrent with the photo-bleaching of DOM optical properties. Photochemical ammonium release was observed in all samples irradiated between four and ten hours, where either linear production or a three step production process was observed with release rates ranging from 0.001 to 3.57 ìM l-1 h-1. Preliminary data indicate that ammonium photo-production is independent of dissolved oxygen and we discuss implications of these findings with regard to the possible mechanism of ammonium photo-production. Photo-chemically induced nitrogen release indicates a new biologically labile source of nitrogen and can impact severely upon the biogeochemistry and nutrient limitation of aquatic environments.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2006
- Bibcode:
- 2006AGUFM.B11C1044S
- Keywords:
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- 0428 Carbon cycling (4806);
- 0452 Instruments and techniques;
- 0478 Pollution: urban;
- regional and global (0345;
- 4251);
- 0496 Water quality;
- 4894 Instruments;
- sensors;
- and techniques