Photochemical oxygen consumption in marine waters: A major sink for colored dissolved organic matter?
TL;DR: In this article, the authors measured apparent quantum yields (AQYs) of photobleaching, O2 uptake, and H2O2 production in several coastal marine samples and in dilutions of a tropical estuarine water with oligotrophic seawater.
read more
Abstract: Quantification of photochemical O 2 uptake provides a measure of total chemical photooxidation of dissolved organic matter (DOM). Here we study this process and present estimates suggesting that photooxidation has the potential to significantly modify marine DOM pools, complementing or exceeding oxidation via coupled chemicalbiological pathways. We measured apparent quantum yields (AQYs) of photobleaching, O2 uptake, and H2O2 production in several coastal marine samples and in dilutions of a tropical estuarine water with oligotrophic seawater. O2-loss AQYs varied little among samples or with dilution but decreased linearly from 1.2 3 10 23 at 300 nm to 0.3 3 10 23 at 400 nm and dropped about threefold to near-constant values with increasing absorbed light dose. H2O2 production, about 45% of O2 uptake, showed similar dependencies, whereas singlet oxygen (O2( 1 Dg)) reactions contributed less than 1% of O2 uptake for typical coastal water. Implications of these findings for photochemical O2 ,H 2O2, and DOM cycling are discussed. Modeling the dose-dependence of O2 loss and photobleaching at 310 nm required three DOM pools. In the simplest case, about 90% is a weakly absorbing, low-AQY pool of DOM admixed with two similar-sized pools of more photochemically reactive DOM. This result suggests that rigorously extrapolating laboratory data to the environment requires detailed mapping of dose-wavelength-photobleaching AQY surfaces. Action spectra and DOM flux estimates for coastal photooxidative chemistry were derived. Site-specific potential rates are comparable to available in situ data. Globally, the DOM photolysis capacity appears to be larger than estimated coastal DOM inputs, especially in tropical and temperate areas, including areas with maximal DOM inputs.
read more
Chat with Paper
AI Agents for this Paper
Find similar papers on Google Scholar, PubMed and Arxiv
Write a critical review of this paper
Analyze citations of this paper to find unaddressed research gaps
Citations
Absorption spectral slopes and slope ratios as indicators of molecular weight, source, and photobleaching of chromophoric dissolved organic matter
John R. Helms,Aron Stubbins,Jason D. Ritchie,Elizabeth C. Minor,David J. Kieber,Kenneth Mopper +5 more
TL;DR: In this article, a new approach for parameterizing dissolved organic matter (DOM) ultraviolet-visible absorption spectra is presented, where two distinct spectral slope regions (275-295 nm and 350-400 nm) within log-transformed absorption spectras were used to compare DOM from contrasting water types, ranging from wetlands (Great Dismal Swamp and Suwannee River) to photobleached oceanic water (Atlantic Ocean).
Chapter 10 – Chromophoric DOM in the Coastal Environment
Neil V. Blough,Rossana Del Vecchio +1 more
- 01 Jan 2002
TL;DR: A discussion on chromophoric dissolved organic matter (DOM) in the coastal environment can be found in this article, where the authors focus on the properties and distribution of the major light-absorbing constituent of the DOM pool in natural waters (the 0.2 μm fraction).
499
Sunlight controls water column processing of carbon in arctic fresh waters
TL;DR: In this paper, the dominant fate of dissolved organic carbon (DOC) released from permafrost soils to inland waters is either complete oxidation to CO2 or partial oxidation and river export to oceans.
482
The Global Distribution and Dynamics of Chromophoric Dissolved Organic Matter
Norman B. Nelson,David A. Siegel +1 more
TL;DR: Significant decadal-scale fluctuations in the abundance of global surface ocean CDOM have been observed using remote sensing, indicating a potentially important role for CDOM in ocean-climate connections through its impact on photochemistry and photobiology.
401
Photochemical and microbial degradation of dissolved lignin phenols: Implications for the fate of terrigenous dissolved organic matter in marine environments
TL;DR: In this article, molecular level characterizations of dissolved lignin were conducted in Mississippi River plume waters to study the impact of various removal mechanisms (photooxidation, microbial degradation, and flocculation) on dissolved organic material (DOM) concentrations and compositions.
References
Oxygen consumption from natural waters by photo-oxidizing processes
TL;DR: In this article, it was shown that 5 to 40% of the oxygen produced by photosynthetically active organisms can be fixed through photochemical reactions, even though they are confined to the surface layer of natural waters.
38
Characterization of natural and synthetic humic substances (melanoidins) by stable carbon and nitrogen isotope measurements and elemental compositions
TL;DR: In this article, stable carbon isotope ratios of the starting sugars and amino acids are mostly preserved in laboratory synthetic melanoidins, indicating that nitrogen fractionation could occur during the rate-determining step in the Maillard reaction.
37
Prediction of Photochemical Transformation of Pollutants in the Aquatic Environment
Richard G. Zepp,George L. Baughman +1 more
- 01 Jan 1978
TL;DR: In this paper, the authors focus on methods for prediction of photolysis by the action of sunlight and use them to assess potential exposure of aquatic organisms to toxic pollutants in natural waters.
33
•Dissertation
Characteristics of photochemical production of carbon monoxide in seawater
George Dean Redden
- 03 Sep 1982
TL;DR: In this paper, the effect of radiation wavelength was studied using cellulose acetate, Mylar, polycarbonate, and yellow acrylic filters to attenuate the middle and near ultraviolet (UV), and blue-green regions of the solar spectrum.