Photoinduced Generation of Hydroxyl Radical in Natural Waters

Author(s):  
Khan M. G. Mostofa ◽  
Cong-qiang Liu ◽  
Hiroshi Sakugawa ◽  
Davide Vione ◽  
Daisuke Minakata ◽  
...  
2016 ◽  
Vol 13 (4) ◽  
pp. 757 ◽  
Author(s):  
Jarod N. Grossman ◽  
Tara F. Kahan

Environmental contextReactions in natural waters such as lakes and streams are thought to be extremely slow in the absence of sunlight (e.g. at night). We demonstrate that in the presence of iron, hydrogen peroxide and certain bacteria (all of which are common in natural waters), certain reactions may occur surprisingly quickly. These findings will help us predict the fate of many compounds, including pollutants, in natural waters at night. AbstractDark Fenton chemistry is an important source of hydroxyl radicals (OH•) in natural waters in the absence of sunlight. Hydroxyl radical production by this process is very slow in many bodies of water, owing to slow reduction and low solubility of FeIII at neutral and near-neutral pH. We have investigated the effects of the iron-reducing bacteria Shewanella oneidensis (SO) on OH• production rates from Fenton chemistry at environmentally relevant hydrogen peroxide (H2O2) and iron concentrations at neutral pH. In the presence of 2.0 × 10–4M H2O2, OH• production rates increased from 1.3 × 10–10 to 2.0 × 10–10Ms–1 in the presence of 7.0 × 106cellsmL–1 SO when iron (at a concentration of 100μM) was in the form of FeII, and from 3.6 × 10–11 to 2.2 × 10–10Ms–1 when iron was in the form of FeIII. This represents rate increases of factors of 1.5 and 6 respectively. We measured OH• production rates at a range of H2O2 concentrations and SO cell densities. Production rates depended linearly on both variables. We also demonstrate that bacteria-assisted Fenton chemistry can result in rapid degradation of aromatic pollutants such as anthracene. Our results suggest that iron-reducing bacteria such as SO may be important contributors to radical formation in dark natural waters.


2014 ◽  
Vol 16 (4) ◽  
pp. 757-763 ◽  
Author(s):  
Luni Sun ◽  
Hongmei Chen ◽  
Hussain A. Abdulla ◽  
Kenneth Mopper

This study showed that hydroxyl radical (˙OH) production during long-term irradiation experiments is most accurately measured using instantaneous rates.


2004 ◽  
Vol 20 (1) ◽  
pp. 153-158 ◽  
Author(s):  
Kazuhiko TAKEDA ◽  
Hiroshi TAKEDOI ◽  
Shuhei YAMAJI ◽  
Keiichi OHTA ◽  
Hiroshi SAKUGAWA

2003 ◽  
Vol 60 (2) ◽  
pp. 203-213 ◽  
Author(s):  
L A Molot ◽  
S A Miller ◽  
P J Dillon ◽  
C G Trick

An assay has been developed to measure extracellular hydroxyl radical (OH*) activity in algal culture media and natural waters over a 4- to 5-day period. The first-order rate constant, k, for loss of absorbance at 590 or 620 nm was determined for erioglaucine, which is sensitive to OH*, insensitive to superoxide and hydrogen peroxide, and stable in the dark and under artificial radiation (280–750 nm) and solar radiation in the absence of oxidants. Variation in irradiance was accounted for by normalizing k with k for a ferric iron reference solution with dye (k/kfe). Trends in k/kfe for streams and lakes were consistent with previous data on photochemical oxidation rates of dissolved organic matter. Values for k/kfe were similar in filtered surface waters of eutrophic Heart Lake and nearby mesotrophic Lake St. George under artificial radiation. Hence, extracellular OH* did not appear to be a direct cause of the onset of a nuisance cyanobacterial bloom in Heart Lake, nor did OH* appear related to the absence of a bloom in Lake St. George. k/kfe was two orders of magnitude higher in algal culture media supplied with 8.8 mM nitrate than in lake waters.


2013 ◽  
Vol 47 (14) ◽  
pp. 5422-5430 ◽  
Author(s):  
Monica Passananti ◽  
Fabio Temussi ◽  
Maria Rosaria Iesce ◽  
Gilles Mailhot ◽  
Marcello Brigante

Chemosphere ◽  
2021 ◽  
pp. 132318
Author(s):  
Zimi Ye ◽  
Zhongyu Guo ◽  
Jieqiong Wang ◽  
Lilan Zhang ◽  
Yuchen Guo ◽  
...  

2004 ◽  
Vol 71 ◽  
pp. 97-106 ◽  
Author(s):  
Mark Burkitt ◽  
Clare Jones ◽  
Andrew Lawrence ◽  
Peter Wardman

The release of cytochrome c from mitochondria during apoptosis results in the enhanced production of superoxide radicals, which are converted to H2O2 by Mn-superoxide dismutase. We have been concerned with the role of cytochrome c/H2O2 in the induction of oxidative stress during apoptosis. Our initial studies showed that cytochrome c is a potent catalyst of 2′,7′-dichlorofluorescin oxidation, thereby explaining the increased rate of production of the fluorophore 2′,7′-dichlorofluorescein in apoptotic cells. Although it has been speculated that the oxidizing species may be a ferryl-haem intermediate, no definitive evidence for the formation of such a species has been reported. Alternatively, it is possible that the hydroxyl radical may be generated, as seen in the reaction of certain iron chelates with H2O2. By examining the effects of radical scavengers on 2′,7′-dichlorofluorescin oxidation by cytochrome c/H2O2, together with complementary EPR studies, we have demonstrated that the hydroxyl radical is not generated. Our findings point, instead, to the formation of a peroxidase compound I species, with one oxidizing equivalent present as an oxo-ferryl haem intermediate and the other as the tyrosyl radical identified by Barr and colleagues [Barr, Gunther, Deterding, Tomer and Mason (1996) J. Biol. Chem. 271, 15498-15503]. Studies with spin traps indicated that the oxo-ferryl haem is the active oxidant. These findings provide a physico-chemical basis for the redox changes that occur during apoptosis. Excessive changes (possibly catalysed by cytochrome c) may have implications for the redox regulation of cell death, including the sensitivity of tumour cells to chemotherapeutic agents.


Sign in / Sign up

Export Citation Format

Share Document