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Published in final edited form as: Atmos Environ (1994). 2012 Jan 1;46:665–668. doi: 10.1016/j.atmosenv.2011.10.006

A Comparison of Hydroxyl Radical and Hydrogen Peroxide Generation in Ambient Particle Extracts and Laboratory Metal Solutions

Huiyun Shen a, Cort Anastasio a,*
PMCID: PMC3259706  NIHMSID: NIHMS334774  PMID: 22267949

Abstract

Generation of reactive oxygen species (ROS) – including superoxide (O2), hydrogen peroxide (HOOH), and hydroxyl radical (OH) – has been suggested as one mechanism underlying the adverse health effects caused by ambient particulate matter (PM). In this study we compare HOOH and OH production from fine and coarse PM collected at an urban (Fresno) and rural (Westside) site in the San Joaquin Valley (SJV) of California, as well as from laboratory solutions containing dissolved copper or iron. Samples were extracted in a cell-free, phosphate-buffered saline (PBS) solution containing 50 μM ascorbate (Asc). In our laboratory solutions we find that Cu is a potent source of both HOOH and OH, with approximately 90% of the electrons that can be donated from Asc ending up in HOOH and OH after 4 h. In contrast, in Fe solutions there is no measurable HOOH and only a modest production of OH. Soluble Cu in the SJV PM samples is also a dominant source of HOOH and OH. In both laboratory copper solutions and extracts of ambient particles we find much more production of HOOH compared to OH: e.g., HOOH generation is approximately 30 – 60 times faster than OH generation. The formation of HOOH and OH are positively correlated, with roughly 3 % and 8 % of HOOH converted to OH after 4 and 24 hr of extraction, respectively. Although the SJV PM produce much more HOOH than OH, since OH is a much stronger oxidant it is unclear which species might be more important for oxidant-mediated toxicity from PM inhalation.

Keywords: particulate matter (PM), reactive oxygen species (ROS), transition metals, copper, iron

1. Introduction

One suggested mechanism by which ambient particulate matter (PM) causes adverse health effects is PM-mediated oxidative stress and cell damage through the generation of reactive oxygen species (ROS) such as superoxide (O2), hydrogen peroxide (HOOH), and hydroxyl radical (OH) (Donaldson et al., 2003; Gonzalez-Flecha, 2004; Li et al., 2008; Valavanidis et al., 2008). ROS can be chemically generated by redox-active transition metals (TM) such as iron (Fe) and copper (Cu), which shuttle electrons from reductants such as ascorbate (Asc) onto dissolved oxygen (Shen et al., 2011). Multiple in vitro and in vivo studies have shown that HOOH can induce cytotoxicity (Hyslop et al., 1988; Oosting et al., 1990), while the highly reactive OH can react with carbohydrates, lipids, proteins, and nucleic acids, resulting in cell death and disease (Valavanidis et al., 2008; Kell, 2010).

Previous studies have shown that Fe and Cu are the most important TMs in chemically generating ROS from ambient particles (Donaldson et al., 1997; Shi et al., 2003; Vidrio et al., 2008; DiStefano et al., 2009; Vidrio et al., 2009; Wang et al., 2010; Shen et al., 2011). These metals are also important in converting HOOH to OH via the Fenton, or Fenton-like, reaction (Valko et al., 2005):

Fe(II)+HOOHFe(III)+OH+OH (1)
Cu(I)+HOOHCu(II)+OH+OH (2)

A number of groups have measured the chemical generation of OH or HOOH from particles extracted in cell-free buffer solutions (Hasson and Paulson, 2003; Shi et al., 2003; Baulig et al., 2004; Arellanes et al., 2006; Jung et al., 2006; Kunzli et al., 2006; Alaghmand and Blough, 2007; DiStefano et al., 2009; Vidrio et al., 2009; Wang et al., 2010). We recently reported the generation of HOOH and, separately, OH by fine and coarse PM collected at an urban and rural site in the San Joaquin Valley (SJV) of California (Shen and Anastasio, 2011; Shen et al., 2011). In order to take advantage of this unique data set, the first where both of these ROS species were measured on the same particle extracts, here we compare our HOOH and OH results in order to examine the relative amounts formed and the efficiency with which HOOH is converted to OH.

2. Materials and methods

Below we briefly describe our experimental techniques; details are available in Shen at al. (2011) and Shen and Anastasio (2011). All experiments were performed in a chelex-100-treated, cell-free surrogate lung fluid (SLF) solution that contained 114 mM NaCl, 7.8 mM Na2HPO4 and 2.2 mM KH2PO4 to buffer the solution at pH 7.2–7.4, and 10 mM sodium benzoate (for OH measurements).

Fine (PM2.5) and coarse (PM2.5–10 or PMcf) particle samples were collected at an urban (Fresno) and rural (Westside) site in California’s SJV during summer and winter between 2006 and 2009. The urban site has abundant vehicular emissions, while the rural site is largely agricultural. For ROS measurements, a punch of PM2.5 filter or a piece of PMcf foil was placed in a Teflon vial containing SLF with 50 μM Asc (an important endogenous antioxidant in lung lining fluid) and shaken in the dark at room temperature for up to 4 h (for HOOH) or 24 h (for OH). The median extracted PM masses in each vial were 56 and 67 μg for PM2.5 and PMcf, respectively. We performed similar measurements using laboratory metal solutions of CuSO4 or FeSO4 in 4 mL of SLF with 50 μM Asc. HOOH was analyzed using HPLC (Kok et al., 1995), while OH was determined with a benzoate probe by HPLC (Jung et al., 2006). The detection limits for HOOH and OH measurements were approximately 20 and 30 nM, respectively. Cu and Fe in the filtered PM extracts were analyzed by ICP-MS.

Two parameters were determined for each ROS species in each sample: (1) the initial rate of formation, calculated using the 0 and 1 h time points, and (2) the maximum formed during the extraction time (i.e., the highest concentration of HOOH measured within 4 h and the total amount of OH formed after 24 h). PM results are normalized by the sampled air volume. Air-volume-normalized Cu concentrations in PM can be converted to aqueous-extract concentrations using

Cu(nM)=Cu(nmol/m3air)×Vair/VSLF (3)

where Vair is the sampled air volume corresponding to the filter punch or foil piece (2.346 m3 for PM2.5 and 21.444 m3 for PMcf) and VSLF is the extract volume (0.004 L for HOOH and 0.006 L for OH). ROS and metal results are adjusted for the volume difference in the HOOH and OH extracts. Data are presented as means ± SD.

3. Results and discussion

3.1. Generation of HOOH and OH from dissolved Cu and Fe

We first measured HOOH and OH formation in laboratory solutions containing Cu(II) (e.g., Figure S1) or Fe(II). For copper solutions, HOOH generation is approximately 20 to 60 times faster than OH generation (Fig. 1A), and the maximum concentration of HOOH formed is 7 to 13 times higher than the total OH formed over 24 h (Fig. 1B). The maxima for both HOOH and OH plateau at higher Cu(II) concentrations (Fig. 1), probably because of depletion of ascorbate. Assuming that all 50 μM Asc is depleted in the 600 nM Cu solution, we can calculate an “electron balance” based on the knowledge that Asc can donate 2 eand that it requires 2 and 3 e, respectively, to form HOOH and OH from dissolved O2. Thus the 41.5 μM of HOOH formed at 4 h from 600 nM Cu (Fig. 1B) represents 83% of the electrons from Asc while the 1.9 μM of OH formed at 4 h (data not shown) corresponds to 6% of the electrons from Asc. Thus ROS formation at high copper concentrations is very efficient, with approximately 90% of the Asc electrons ending up in HOOH and OH after 4 h.

Figure 1.

Figure 1

Figure 1

Initial rate of ROS formation (panel A) and maximum ROS formed (panel B) as a function of soluble metal concentration in SLF with 50 μM ascorbate. The HOOH data for copper is from Shen et al. (2011). Regression equations are given in the Supplementary data.

In contrast, Fe(II) generates very low concentrations of OH, with an initial rate approximately 20 times lower than for Cu, and makes no measurable HOOH (Fig. 1). By 4 h the OH concentration from 500 nM Fe(II) is 0.16 μM (data not shown), representing only 0.5% of the initial ascorbate electrons.

However, while Cu is a much more potent source of HOOH and OH than Fe in these laboratory solutions, the reactivity of both of these metals depends strongly on the composition of the surrogate lung fluid. In the SLF used in our current experiments, with Asc as the only antioxidant, Cu is much more efficient than Fe at making OH (Vidrio et al., 2008; Charrier and Anastasio, 2011). However, the presence of other physiologically important compounds can both suppress OH generation from Cu and enhance OH from Fe (Vidrio et al., 2008; Charrier and Anastasio, 2011).

3.2. Generation of HOOH and OH from ambient particles

The initial rates of formation of HOOH and OH in the Fresno particle extracts are both strongly linearly correlated with the SLF-soluble Cu concentrations (Fig. 2). In these ambient PM extracts, HOOH generation is approximately 30 times faster than OH generation at a given copper level (Fig. 2), in general agreement with our laboratory Cu solution results (Fig. 1A). The maximum amounts of HOOH and OH generated in the particle extracts are also strongly, though non-linearly, related to soluble copper, with approximately 10 times more HOOH formed than OH (Fig. S2). That is, over the 24 h of extraction, approximately 10% of the HOOH formed was converted to OH. In contrast to these strong correlations for the Fresno particles, we found no correlation between Cu and ROS formation by Westside PM.

Figure 2.

Figure 2

Correlations between the initial rates of HOOH and OH formation and soluble Cu in SJV PM extracts. Regressions: y = 60x + 2.7, R2=0.82 for HOOH (Shen et al., 2011) and y = 2.1x + 0.03, R2=0.98 for OH (Shen and Anastasio, 2011). See Equation (3) for converting the air-volume-normalized Cu concentrations in PM to aqueous extract concentrations.

The initial rates of HOOH and OH formation in the Fresno particle extracts are well correlated, with approximately 3% of HOOH being converted to OH at short times (Fig. 3). The maximum amounts of HOOH and OH in the Fresno PM extracts are also positively correlated, with approximately 8% of HOOH converted to OH over 24 h (Fig. S3).

Figure 3.

Figure 3

Correlation between the initial rates of OH and HOOH formation from SJV PM. The linear correlation for the Fresno PM is y = 0.025x + 0.046, R2 = 0.75.

3.3. Factors influencing the OH/HOOH ratio

In this last section we examine whether the relative amounts of OH and HOOH generated by laboratory solutions and ambient particle extracts depend on the amounts of soluble copper and/or iron. As our diagnostic parameters, we use the ratio of the initial rates of OH and HOOH formation (“rate ratio”) and the ratio of the maximum amounts formed (“max ratio”), both expressed as OH/HOOH.

Figure 4 shows the relationship between the OH/HOOH ratios versus the SLF-soluble Cu concentration in both lab solutions and PM extracts. The two lines show the calculated rate ratio (dashed) and max ratio (solid), respectively, based on our Cu solution data. In these lab solutions the rate ratios (0.018 – 0.022), measured within the first hour of extraction, are much lower than the max ratios (0.080 – 0.225), measured later, reflecting the fact that HOOH generally peaks within a few hours during extraction (Shen et al., 2011), while the total OH increases throughout the 24 h of extraction (Shen and Anastasio, 2011). Compared to the laboratory copper solutions, the OH/HOOH ratios in the SJV PM extracts are higher by average factors of 3.1 (for rate ratio) and 1.8 (for max ratio). This suggests that species in ambient particles enhance the conversion of HOOH to OH. In addition, the max ratios for OH/HOOH are higher when the soluble Cu concentration is lower (below 100 nM), suggesting more efficient conversion of HOOH to OH at lower copper concentrations (Fig. 4). We calculate that the typical Cu concentration in human lung lining fluid from inhalation of Fresno PM is 100 nM (73% from PM2.5), based on an average adult lung lining fluid volume of 25 mL, an inhaled air volume of 20 m3 per day, assuming 30% and 70% of inhaled fine and coarse PM deposit in the lung, respectively, and using our Fresno median Cu mass concentrations of 19.5 and 3.2 ng m−3 for PM2.5 and PMcf, respectively (Shen et al., 2011). The Westside particles, with low Cu concentrations, generally have higher OH/HOOH values (Fig. 4), although they generate much lower absolute amounts of OH and HOOH than the Fresno PM (Fig. 2).

Figure 4.

Figure 4

The ratio of OH formation over HOOH formation as a function of soluble Cu. The rate ratio and max ratio from both the lab solutions and the SJV PM extracts are shown. The two lines show the calculated rate ratio (dashed) and max ratio (solid) based on the lab solution data (Fig. 1).

Figure 5 shows that a higher soluble Fe/Cu ratio is also associated with a higher OH/HOOH ratio, i.e., with more efficient conversion of HOOH to OH. Part of this relationship is probably due to higher OH/HOOH ratios at lower copper amounts (Figs. 4, S4A, and S4C). However, while the SLF-soluble Fe amount does not seem to affect OH/HOOH directly (Fig. S4B and S4D), higher OH/HOOH values at higher Fe/Cu ratios (Fig. 5) is consistent with the fact that Fe(II) converts HOOH to OH via the Fenton reaction (R1).

Figure 5.

Figure 5

Ratios of OH over HOOH as a function of the soluble Fe/Cu ratio in PM extracts. The regression equations are: y = 0.029Ln(x) + 0.050, R2 = 0.57 for the rate ratio (dashed line) and y = 0.103Ln(x) + 0.197, R2 = 0.52 for the max ratio (solid line).

4. Conclusion

In cell-free solutions containing ascorbate, Cu is a very efficient source of HOOH and OH, while Fe is a modest source of OH. Both Cu solutions and urban (Fresno, CA) particles generate much more HOOH than OH, and levels of these ROS are positively correlated. The conversion of HOOH to OH is generally more efficient at lower Cu concentrations and higher Fe/Cu ratios.

Supplementary Material

01

Acknowledgments

We thank Yongjing Zhao, Walter Ham, Mike Kleeman, Chris Ruehl, Norman Kado, and Yuee Pan for PM samples and Jessie Charrier for HOOH measurements from Fe. This research was funded by the U.S. EPA (RD-83241401-0) through the San Joaquin Valley Aerosol Health Effects Research Center at UC Davis. Additional funding was provided by the California Agricultural Experiment Station (Project CA-D*-LAW-6403-RR) and the NIEHS (P42ES004699).

Footnotes

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References

  1. Alaghmand M, Blough NV. Source-dependent variation in hydroxyl radical production by airborne particulate matter. Environmental Science & Technology. 2007;41:2364–2370. doi: 10.1021/es061902o. [DOI] [PubMed] [Google Scholar]
  2. Arellanes C, Paulson SE, Fine PM, Sioutas C. Exceeding of Henry's law by hydrogen peroxide associated with urban aerosols. Environmental Science & Technology. 2006;40:4859–4866. doi: 10.1021/es0513786. [DOI] [PubMed] [Google Scholar]
  3. Baulig A, Poirault JJ, Ausset P, Schins R, Shi TM, Baralle D, Dorlhene P, Meyer M, Lefevre R, Baeza-Squiban A, Marano F. Physicochemical characteristics and biological activities of seasonal atmospheric particulate matter sampling in two locations of Paris. Environmental Science & Technology. 2004;38:5985–5992. doi: 10.1021/es049476z. [DOI] [PubMed] [Google Scholar]
  4. Charrier JG, Anastasio C. Impacts of antioxidants on hydroxyl radical production from individual and mixed transition metals in a surrogate lung fluid. Atmospheric Environment. 2011 doi: 10.1016/j.atmosenv.2010.12.021. In press. [DOI] [PMC free article] [PubMed] [Google Scholar]
  5. DiStefano E, Eiguren-Fernandez A, Delfino RJ, Sioutas C, Froines JR, Cho AK. Determination of metal-based hydroxyl radical generating capacity of ambient and diesel exhaust particles. Inhalation Toxicology. 2009;21:731–738. doi: 10.1080/08958370802491433. [DOI] [PubMed] [Google Scholar]
  6. Donaldson K, Brown DM, Mitchell C, Dineva M, Beswick PH, Gilmour P, MacNee W. Free radical activity of PM10: iron-mediated generation of hydroxyl radicals. Environmental Health Perspectives. 1997;105:1285–1289. doi: 10.1289/ehp.97105s51285. [DOI] [PMC free article] [PubMed] [Google Scholar]
  7. Donaldson K, Stone V, Borm PJ, Jimenez LA, Gilmour PS, Schins RP, Knaapen AM, Rahman I, Faux SP, Brown DM, MacNee W. Oxidative stress and calcium signaling in the adverse effects of environmental particles (PM10) Free Radical Biology and Medicine. 2003;34:1369–1382. doi: 10.1016/s0891-5849(03)00150-3. [DOI] [PubMed] [Google Scholar]
  8. Gonzalez-Flecha B. Oxidant mechanisms in response to ambient air particles. Molecular Aspects of Medicine. 2004;25:169–182. doi: 10.1016/j.mam.2004.02.017. [DOI] [PubMed] [Google Scholar]
  9. Hasson AS, Paulson SE. An investigation of the relationship between gas-phase and aerosol-borne hydroperoxides in urban air. Journal of Aerosol Science. 2003;34:459–468. [Google Scholar]
  10. Hyslop PA, Hinshaw DB, Halsey WA, Jr, Schraufstatter IU, Sauerheber RD, Spragg RG, Jackson JH, Cochrane CG. Mechanisms of oxidant-mediated cell injury. The glycolytic and mitochondrial pathways of ADP phosphorylation are major intracellular targets inactivated by hydrogen peroxide. The Journal of Biological Chemistry. 1988;263:1665–1675. [PubMed] [Google Scholar]
  11. Jung H, Guo B, Anastasio C, Kennedy IM. Quantitative measurements of the generation of hydroxyl radicals by soot particles in a surrogate lung fluid. Atmospheric Environment. 2006;40:1043–1052. [Google Scholar]
  12. Kell DB. Towards a unifying, systems biology understanding of large-scale cellular death and destruction caused by poorly liganded iron: Parkinson's, Huntington's, Alzheimer's, prions, bactericides, chemical toxicology and others as examples. Archives of Toxicology. 2010;84:825–889. doi: 10.1007/s00204-010-0577-x. [DOI] [PMC free article] [PubMed] [Google Scholar]
  13. Kok GL, McLaren SE, Staffelbach TA. HPLC determination of atmospheric organic hydroperoxides. Journal of Atmospheric and Oceanic Technology. 1995;12:282–289. [Google Scholar]
  14. Kunzli N, Mudway IS, Gotschi T, Shi T, Kelly FJ, Cook S, Burney P, Forsberg B, Gauderman JW, Hazenkamp ME, Heinrich J, Jarvis D, Norback D, Payo-Losa F, Poli A, Sunyer J, Borm PJ. Comparison of oxidative properties, light absorbance, total and elemental mass concentration of ambient PM2.5 collected at 20 European sites. Environmental Health Perspectives. 2006;114:684–690. doi: 10.1289/ehp.8584. [DOI] [PMC free article] [PubMed] [Google Scholar]
  15. Li N, Xia T, Nel AE. The role of oxidative stress in ambient particulate matter-induced lung diseases and its implications in the toxicity of engineered nanoparticles. Free Radical Biology and Medicine. 2008;44:1689–1699. doi: 10.1016/j.freeradbiomed.2008.01.028. [DOI] [PMC free article] [PubMed] [Google Scholar]
  16. Oosting RS, van Bree L, van Iwaarden JF, van Golde LM, Verhoef J. Impairment of phagocytic functions of alveolar macrophages by hydrogen peroxide. American Journal of Physiology. 1990;259:L87–L94. doi: 10.1152/ajplung.1990.259.2.L87. [DOI] [PubMed] [Google Scholar]
  17. Shen H, Anastasio C. Formation of hydroxyl radical from San Joaquin Valley particles extracted in a cell-free solution. Atmospheric Chemistry and Physics. 2011 doi: 10.5194/acp-11-9671-2011. Submitted. [DOI] [PMC free article] [PubMed] [Google Scholar]
  18. Shen H, Barakat AI, Anastasio C. Generation of hydrogen peroxide from San Joaquin Valley particles in a cell-free solution. Atmospheric Chemistry and Physics. 2011;11:753–765. doi: 10.5194/acp-11-9671-2011. [DOI] [PMC free article] [PubMed] [Google Scholar]
  19. Shi T, Knaapen AM, Begerow J, Birmili W, Borm PJ, Schins RP. Temporal variation of hydroxyl radical generation and 8-hydroxy-2'-deoxyguanosine formation by coarse and fine particulate matter. Occupational and Environmental Medicine. 2003;60:315–321. doi: 10.1136/oem.60.5.315. [DOI] [PMC free article] [PubMed] [Google Scholar]
  20. Valavanidis A, Fiotakis K, Vlachogianni T. Airborne particulate matter and human health: toxicological assessment and importance of size and composition of particles for oxidative damage and carcinogenic mechanisms. Journal of Environmental Science and Health, Part C: Environmental Carcinogenesis and Ecotoxicology Reviews. 2008;26:339–362. doi: 10.1080/10590500802494538. [DOI] [PubMed] [Google Scholar]
  21. Valko M, Morris H, Cronin MTD. Metals, toxicity and oxidative stress. Current Medicinal Chemistry. 2005;12:1161–1208. doi: 10.2174/0929867053764635. [DOI] [PubMed] [Google Scholar]
  22. Vidrio E, Jung H, Anastasio C. Generation of hydroxyl radicals from dissolved transition metals in surrogate lung fluid solutions. Atmospheric Environment. 2008;42:4369–4379. doi: 10.1016/j.atmosenv.2008.01.004. [DOI] [PMC free article] [PubMed] [Google Scholar]
  23. Vidrio E, Phuah CH, Dillner AM, Anastasio C. Generation of hydroxyl radicals from ambient fine particles in a surrogate lung fluid solution. Environmental Science & Technology. 2009;43:922–927. doi: 10.1021/es801653u. [DOI] [PMC free article] [PubMed] [Google Scholar]
  24. Wang Y, Arellanes C, Curtis DB, Paulson SE. Probing the source of hydrogen peroxide associated with coarse mode aerosol particles in Southern California. Environmental Science & Technology. 2010;44:4070–4075. doi: 10.1021/es100593k. [DOI] [PubMed] [Google Scholar]

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