With the aim to assess the effect of possible O-2(.-) generation during an
oxidative burst on O-3 reduction in mesophyll cell walls due to the reactio
n O-2(.-) + O-3 --> O-3(.-) + O-2 and subsequent formation of (OH)-O-., O-3
flow through this sequence was compared with O-2(.-) flow through the comp
etitive sequences where H2O2 is formed. The two-electron reduction of O-3 v
ia the direct reaction with ascorbate was also considered. The calculations
were exemplified in an experiment where Phaseolus vulgaris L. leaves were
exposed to 530 nl O(3)l(-1) in air for 3.5 h. During the exposure, H2O2 was
assumed to be generated at peak rates observed in pathogen-elicited cell s
uspensions. O-3 reduction through reaction with O-2(.-) was 25-44% of O-3 d
etoxified in the direct reaction with ascorbate. More than 99% of O-2(.-) w
as reduced to H2O2 via spontaneous disproportionation and reduction with as
corbate, the disproportionation prevailing at pH 5 and reduction at the exp
ense of ascorbate at pH 7. H2O2 was estimated to be channelled mostly to th
e peroxidase-catalysed scavenging reaction. Calculated steady state H2O2 co
ncentrations were 40-80 mu M. It is concluded that generation of H2O2 at th
e postulated rate was too high and that the generation of O-2(.-) during an
oxidative burst is ineffective in reducing O-3 through the network of reac
tive oxygen species. Superoxide dismutase induction in the cell wall under
O-3 is discussed.