1O2 formation and direct photolysis due to increased absorption by the
substrates (See Table S1. ESI{). Quantum yields of single chromophores
are generally wavelength independent, and are thus applicable to
environmental systems.26
1 D. J. Repeta, N. T. Hartman, S. John, A. D. Jones and R. Goericke,
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Scheme 1 Conversion of 29-Cl-BPA to BPA in photolyses conducted in
EtOH at 254 nm. The quantum yield of dechlorination was calculated as
the percent yield of BPA multiplied by the total direct photolysis W.
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Organic Chemistry, CRC Press, Inc., Boca Raton, FL, 1994.
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The photoreactivity of both 2,4-DCBA and the CBPAs in the
aquatic environment depends not only on their quantum yields of
1O2 formation and direct photolysis, but also on their ability to
absorb solar radiation. The chlorine substituents on 2,4-DCBA
increase the efficiency of 1O2 formation, but also cause the
absorption to undergo a bathochromic shift relative to BA,
allowing for greater solar radiation absorption. Similarly, the
biphenyl compounds generally absorb longer wavelengths more
efficiently than the phenyl compounds. The absorbance of both
29-Cl-BPA and PCB-47 above 300 nm, however, is substantially
less than the other biphenyl compounds due to the non-planarity
of the molecules, and thus the amount of solar radiation absorbed
by biphenyl compounds containing ortho-substituents is expected
to be diminished relative to biphenyl compounds with other
substitution patterns.
This work suggests that chlorinated benzoic and biphenyl
carboxylic acids, if present in the marine environment at the levels
found by Repeta et al., will be significant sources for photo-
1
1
chemically generated O2. Based on the W of O2 formation by
samples of marine CDOM (y0.0611), the W of 1O2 production by
2,4-DCBA, and assuming 2,4-DCBA is responsible for 2% of the
total absorbance by CDOM, this single chromophore would
1
account for approximately 15% of the O2 generated by marine
CDOM. This work also indicates that these compounds are
weakly photolabile, which should lead to vertical concentration
gradients as they are depleted from marine surface waters.
Additionally, the magnitude of 1O2 formation will depend on
the substitution pattern, as any CBPA containing ortho-chlorine
substituents absorb less solar radiation, and are expected to
undergo chlorine loss in conjunction with sensitization of 1O2.
Their degradation products as well as the other isomers of CBPAs
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1
and BPA itself, however, are also efficient O2 sensitizers.
Notes and references
{ The use of wavelengths shorter than 300 nm (266 and 254 nm), although
not environmentally relevant, were used to calculate the quantum yields of
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Chem. Commun., 2005, 4113–4115 | 4115