A study of the pH profile ofthe decomposition of aqueous hypochlorite has revealed the evolution (onset at pH 8) of single (1A g) molecular oxygen (singlet spin state dioxygen) detected spectroscopically (1268 nm), prior to the appearance of chlorine (onset at pH 5.5). The possible mechanism of the singlet state dioxygen evolution is presented, and the origin of its chloride ion dependence is discussed, especially in reference to chloride ion dependence of singlet molecular oxygen evolution in biological systems. Recent epidemiological analyses of the correlation of human cancer with chlorinated water supplies focus attention on the singlet oxygen mechanisms of DNA lesion formation.
Singlet Molecular Oxygen GenerationIn a general study of singlet molecular oxygen generation, we discovered that simple acidification of hypochlorite solutions yielded typical IR emission characteristic of singlet molecular (excited) oxygen. Currently, an epidemiological study (1) has correlated the statistics of human cancer with use of chlorinated water supply. The demonstration of singlet oxygen attack on DNA components by several laboratories (2-4) suggests a possible mechanistic role for the singlet oxygen generated in acidic environments in the correlation between chlorinated water and cancer.A study of the pH profile of the decomposition of aqueous hypochlorite has revealed the evolution (onset at pH 8) of singlet ('Ag) molecular oxygen (singlet spin state dioxygen) detected spectroscopically (1268 nm), prior to the appearance of chlorine (onset at pH 5.5). This result is surprising because it has been overlooked in the long history of research on the chlorine-hypochlorite equilibria, kinetics, and mechanisms. These observations suggest another focus on mechanisms of redox reactions involving H202 and singlet oxygen species, in both chemical and biological systems.
Experimental Results on Acidification of HypochloriteThe generation of singlet molecular oxygen by the chemiluminescent reaction of hydrogen peroxide with aqueous hypochlorite is well known and is now a standard method (5-9), HOOH + OCF --10* + HOH + Cl-, [1] the singlet oxygen being detected spectroscopically. Initially, this was observed (5, 6) as the 634-nm simultaneous transition(1'A5,) (lAg) -_ (3X ) (3k-) for the electron exchange collision of excited molecular pairs. The preferred and more efficient method is the direct detection of the lAg 31 emission at 1268 nm in the near infrared, and this method (10, 11) has been used in the present research. We used a Ge-photodiode detector with a dedicated near-IR spectrometer in the 1-to 1.7-gm region, with electronic and data-processing peripherals (12). Fig. 1 shows the typical 1268-nm chemiluminescence spectra recorded upon the acidification of aqueous hypochlorite with HCI at room temperature.The pH profiles of 102 and C12 evolution upon acidification of aqueous hypochlorite solution at room temperature are shown in Fig. 2 (reagent-grade sodium hypochlorite solution, acidified by reagent grade hydrochloric...