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1987, ACS Symposium Series
Sunlight that arrives at the surface of the earth contains substantial amounts of energy. When surface waters, which contain either natural or anthropogenic chromophores, are exposed to sunlight, light initiated chemical reactions often occur. Sunlight induced photochemical reactions in surface waters may broadly be defined as environmental aquatic photochemistry. Within aquatic photochemistry, it is possible to envision reactions involving either inorganic and/or organic molecules. These chemicals could be either natural or anthropogenic and may participate in either homogeneous or heterogeneous reactions. Very often in these environments, a complex array of primary and secondary photoprocesses are occurring simultaneously. Surface waters are diverse in nature. They might be near shore or inland wetland environments or mid-oceanic oligotrophic water. Until recently, sunlight induced photochemistry was not recognized as an important pathway for the transformation of natural and anthropogenic chemicals in surface waters. It is now well established that photochemically mediated processes are important in most, if not all, areas of aqueous phase environmental chemistry. Both direct, primary, and indirect photoprocesses have been documented in natural waters.
Environmental Science & Technology, 1984
Photochemical reactions may affect the photic zone, the surface sunlit layer of freshwaters, oceans, and estuarine regimes where fresh and saltwaters begin to interact. Hydrosphere photochemistry influences the world's oceans (about 70% of the Earth's surface), and the illuminated portion of the hydrosphere is especially active and diverse. 'Ransport, material exchanges, and biology (including aquatic primary pro-3 S A Environ. Sci.Technol.
Chemistry-a European Journal, 2014
This paper gives an overview of the main reactive transient species that are produced in surface waters by sunlight illumination of photoactive molecules (photosensitizers), such as nitrate, nitrite, and chromophoric dissolved or-ganic matter (CDOM). The main transients (COH, CO 3 À C, 1 O 2 , and CDOM triplet states) are involved in the indirect phototransformation of a very wide range of persistent organic pollutants in surface waters.
Comprehensive Series in Photochemical & Photobiological Sciences, 2015
Book: Photochemical processes taking place in surface waters, role of natural organic matter in photochemical reactions and to recently developed tools, analytical techniques Chapter 3. CHARACTERISTICS OF THE UNDERWATER LIGHT FIELD
Aquatic Sciences - Research Across Boundaries, 2003
The importance of solar-driven processes in the hydrosphere has become increasingly evident over the past decade. The absorption of sunlight by both natural and anthropogenic chromophores within natural waters can initiate a variety of environmentally important photochemical processes. These processes can include: 1) the direct and sensitized phototransformation of anthropogenic organic, organometallic and inorganic compounds; 2) the light-induced weathering of minerals and the lightinduced redox cycling of dissolved metals, thereby influencing metal speciation; 3) photobleaching of the chromophore containing constituents of natural dissolved organic matter, thus altering the aquatic light field and the remote sensing of ocean color. Solar-driven processes also greatly affect the biogeochemical cycles of carbon, nitrogen, phosphorus, and sulfur. Photochemistry can be strongly linked to biological processes, most evident in biological photosynthesis, but also through the production and biological uptake of available forms of nutrients and of trace metals that are essential and/or toxic. Furthermore, many photochemical reactions occur at interfaces, e. g., at the particle-water interface or at the airwater interface, and can affect the production and consumption of atmospherically important trace gases. This special issue of Aquatic Sciences is based largely on contributions to the Symposium "Impact of Photochemical Processes in the Hydrosphere" that was co-organized by Neil V. Blough and Richard G. Zepp at the 225 th American Chemical Society Meeting (New Orleans, March 23-27, 2003). The ten articles published in this special issue
2019
Perspectives on photochemically generated reactive species in the environment, with particular emphasis on the hydrosphere was presented in Chapter 1. The role of solar radiation to provide needed light energy to drive many photochemical reactions involving; geogenic, biogenic and anthropogenic chemicals from the atmosphere and land, found in natural surface waters, was emphasized. A concise definition of reactive species, and discussion of major pathways to their photogeneration were also presented in this chapter. Environmental implications of photogenerated reactive species such as; redox reaction involving ions, dissolved oxygen recycling, generation of secondary reactive species, and photo-degradation of dissolved organic pollutants in natural waters, amongst others were highlighted. Potential technological applications of photochemical generation of reactive species in gas-phase photo-oxidation and photomicrobicidal systems were also mentioned. Chapter 2 reports about concurre...
2013
Information concerning the link between surfacewater photochemistry and climate is presently very scarce as only a few studies have been dedicated to the subject. On the basis of the limited knowledge that is currently available, the present inferences can be made as follows: (1) Warming can cause enhanced leaching of ionic solutes from the catchments to surface waters, including cations and more biologically labile anions such as sulphate. Preferential sulphate biodegradation followed by removal as organic sulphides in sediment could increase alkalinity, favouring the generation of the carbonate radical, CO 3 ·− . However, this phenomenon would be easily offset by fluctuations of the dissolved organic carbon (DOC), which is strongly anticorrelated with CO 3 ·− . Therefore, obtaining insight into DOC evolution is a key issue in understanding the link between photochemistry and climate. (2) Climate change could exacerbate water scarcity in the dry season in some regions. Fluctuations in the water column could deeply alter photochemistry that is usually favoured in shallower waters. However, the way water is lost would strongly affect the prevailing photoinduced processes. Water outflow without important changes in solute concentration would mostly favour reactions induced by the hydroxyl and carbonate radicals (·OH and CO 3 ·− ). In contrast, evaporative concentration would enhance reactions mediated by singlet oxygen ( 1 O 2 ) and by the triplet states of chromophoric dissolved organic matter ( 3 CDOM*). (3) In a warmer climate, the summer stratification period of lakes would last longer, thereby enhancing photochemical reactions in the epilimnion but at the same time keeping the hypolimnion water in the dark for longer periods.
Marine Chemistry, 1987
Glyoxylic and pyruvic acids were formed when filter-sterilized seawater was exposed to solar radiation. Production rates varied from samples collected from distinctly different regions of the sea. Humic-rich seawater from the Florida Bay exhibited net photochemical production rates (glyoxylate, 27.5nM/W-hm 2;pyruvate, 12.9nM/W-hm 2) that were significantly greater than net production rates for humic-poor water (glyoxylate, 3.1nM/W-hm-2; pyruvate, 1.8nM/W-hm 2) collected in the Gulf Stream. When seawater was not filtered, the concentrations of glyoxylate and pyruvate were found to undergo diurnal variations resulting from an imbalance between biological and photochemical processes. A depth profile of the glyoxylate concentration from several oceanic stations showed a pronounced daytime maximum in the upper 10 m; this finding is consistent with laboratory results that demonstrated that glyoxylate is formed photochemically in seawater. Pyruvate, in contrast, showed no clear trend with depth; its distribution in the water column may be primarily controlled by biological processes rather than by photochemical processes. Biological processes are generally thought to control the spatial and temporal distribution of simple organic metabolites in seawater. Our results show that photochemical processes may also be important in the marine cycling of some biochemical compounds.
Water research, 2015
Chromophoric dissolved organic matter (CDOM) in surface waters is a photochemical source of several transient species such as CDOM triplet states ((3)CDOM*), singlet oxygen ((1)O2) and the hydroxyl radical (OH). By irradiation of lake water samples, it is shown here that the quantum yields for the formation of these transients by CDOM vary depending on the irradiation wavelength range, in the order UVB > UVA > blue. A possible explanation is that radiation at longer wavelengths is preferentially absorbed by the larger CDOM fractions, which show lesser photoactivity compared to smaller CDOM moieties. The quantum yield variations in different spectral ranges were definitely more marked for (3)CDOM* and OH compared to (1)O2. The decrease of the quantum yields with increasing wavelength has important implications for the photochemistry of surface waters, because long-wavelength radiation penetrates deeper in water columns compared to short-wavelength radiation. The average steady-...
Inhibitory effect of dissolved organic matter on triplet-induced oxidation of aquatic contaminants
Photochemical & Photobiological Sciences, 2014
Photochemical degradation of dissolved organic matter (DOM) plays an important role in the carbon cycle. Irradiation experiments were conducted to evaluate the influence of chemical factors, specifically those expected to be altered in natural waters by atmospheric acid deposition, on photodegradation of DOM. These included pH, nitrate, iron and calcium. The experiments were carried out using stream and lake water samples with a wide range of dissolved organic carbon (DOC) concentration. Decreasing DOC concentration along with decreasing absorbance was observed during three-week exposures to natural solar radiation as well as during laboratory experiments with artificial solar radiation. The pH of the samples significantly affected degradation rates of DOM especially with elevated iron, while no influence of nitrate or calcium concentration was observed. Addition of Fe III did not significantly affect photodegradation and photobleaching rate constants in samples at circumneutral pH. Acid pH increased photodegradation rates. The results suggest that photodegradation rates of DOM will decrease during recovery from acidification. Hence, lower photodegradation rates may be responsible for increases in DOM observed in some regions of North America and Europe. † Electronic supplementary information (ESI) available. See
Halogenated organic compounds, also termed organohalogens, were initially regarded to be of almost exclusively anthropogenic origin. However, recent research has demonstrated that photochemical reactions are important abiotic sources of organohalogen compounds in sunlit surface waters. Halide ions (X − , X represents Cl, Br and I) are common anions in natural waters and might be oxidized by reactive species originated from photochemistry of dissolved organic matter (DOM) or inorganic photoactive species. The resulting reactive halogen species may react with organic substances with diverse bimolecular reaction rate constants, depending on the complexity and structure of organic substances. Therefore, the chemical mechanism of halogenation remains challenging to be fully elucidated. To better understand the trends in the existing data and to identify the knowledge gaps that may merit further investigation, this review gives an integrative summary on the sources of reactive oxygen species (ROS) and halogen radicals (X • /X 2 • −). Photochemical halogenation of phenolic compounds and formation of methyl halide and brominated organic pollutants are highlighted. By evaluating existing literature and identifying some uncertainties, this review emphasizes the environmental significance of sunlight-driven halogenation and proposes further research directions on mechanistic investigation and rational experimental design close to natural systems.
Catalysis Today, 2007
Solar-light reaching the earth surface is able to induce chemical reactions in absorbing chemicals. For many organic pollutants dispersed in surface waters, photolysis is an important transformation process. It results from absorption of light by the chemical itself or it is mediated by sensitizing or photoinducing chromophores contained in surface waters. Coloured dissolved organic matter (cDOM) and nitrate ions are among these. This paper gives a brief description of major photochemical processes that may occur in surface waters. It is illustrated by three examples of light induced pollutant transformation. The high volume chemical 1-naphthol and the herbicides methabenzthiazuron and mesotrione were chosen as substrates. Analytical and kinetic aspects of the reactions are reported. #
2012
Photoinduced processes, caused by natural sunlight, are key functions for sustaining all living organisms through production and transformation of organic matter (OM) in the biosphere. Production of hydrogen peroxide (H 2 O 2 ) from OM is a primary step of photoinduced processes, because H 2 O 2 acts as strong reductant and oxidant. It is potentially important in many aquatic reactions, also in association with photosynthesis.Allochthonous and autochthonous dissolved organic matter (DOM) can be involved into several photoinduced or biological processes. DOM subsequently undergoes several physical, chemical, photoinduced and biological processes, which can be affected by global warming. This book is uniquely structured to overview some vital issues, such as: DOM; H 2 O 2 and ROOH; HO • ; Degradation of DOM; CDOM, FDOM; Photosynthesis; Chlorophyll; Metal complexation, and Global warming, as well as their mutual interrelationships, based on updated scientific results.
Environmental science. Processes & impacts, 2014
The APEX software predicts the photochemical transformation kinetics of xenobiotics in surface waters as a function of: photoreactivity parameters (direct photolysis quantum yield and second-order reaction rate constants with transient species, namely ˙OH, CO₃(-)˙, (1)O₂ and the triplet states of chromophoric dissolved organic matter, (3)CDOM*), water chemistry (nitrate, nitrite, bicarbonate, carbonate, bromide and dissolved organic carbon, DOC), and water depth (more specifically, the optical path length of sunlight in water). It applies to well-mixed surface water layers, including the epilimnion of stratified lakes, and the output data are average values over the considered water column. Based on intermediate formation yields from the parent compound via the different photochemical pathways, the software can also predict intermediate formation kinetics and overall yield. APEX is based on a photochemical model that has been validated against available field data of pollutant photo...
Biogeochemistry of Marine Dissolved Organic Matter, 2015
Environmental Science & Technology
Photochemical processes appear to have an important impact on the cycling of dissolved organic matter (DOM) in a wide variety of aquatic environments. Numerous photoproducts of DOM, including dissolved inorganic carbon and low-molecular-weight organic compounds, have been identified, and the types of photoproducts and extent of phototransformation of DOM are dependent upon its chemical composition. Heterotrophic bacteria are the primary consumers of DOM, and photochemical transformations of DOM can affect its bacterial utilization in a variety of ways. Numerous studies spanning fresh and marine waters have demonstrated enhanced bacterial growth following exposure of DOM to solar radiation. These studies indicate that photochemical processes can enhance the microbial utilization of biorefractory DOM. Other studies in fresh and marine waters, however, have demonstrated that exposure of DOM to solar radiation can result in a reduction in bacterial growth rates, suggesting that photochemical and microbial processes "compete" for the same substrates. It appears that some photoproducts of DOM are resistant to microbial degradation, suggesting that photochemical processes could be involved in the production as well as destruction of biorefractory DOM.
Reviews of Geophysics, 1987
The area of marine photoc•emistry ubiquitous they have received a great deal of has advanced dramatically during the last four at tention in recent years being the subject of years. The incre_ase in meetings dedicated to the recent reviews on their structure, photophysics, subject and in related publications oes a clear photochemistry and free radical character sign of the growing interest and importance of the topic. The experimental approaches, mechanistic process description and quantitative estimation of photo-processes have become far more sophisticated and detailed than before. A clearer recognition has emerged on the role and importance of p•otochemistry in affecting the biota, chemical speciation and degradation, and atmospheric sources. glucinol based polymer from a benthic marine Copyright 1987 by the American Geophysical Union. macrophyte. Although riboflavin photochemically degraded rapidly to lumichrome and other minor Paper number 7R0317. products it was a far more efficient sensitizer 8755-1209/87/007R-0317515.00 than the other t•o tested. Dunlap and Susic
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