The formation of I atom and Criegee intermediate (CH
2OO) in the reaction of CH
2I with O
2 has potential relevance for aerosol and organic acid production in the marine boundary layer. We report measurements of the absolute yield of I atom as a function of pressure for N
2, He, and O
2 buffer at 298 K. Although the overall rate coefficient is pressure-independent, the I-atom yield, correlated with CH
2OO, decreases with total pressure, presumably because of increased stabilization of CH
2IOO. The extrapolated yield of the I + Criegee channel under tropospheric conditions is small but nonzero, 0.04. The zero-pressure limiting I-atom yield is unity, within experimental error, implying negligible branching to IO + CH
2O. The apparent collision efficiency of O
2 in stabilizing CH
2IOO is a remarkable factor of 13 larger than that of N
2, which suggests unusually strong interaction or possible reaction between the chemically activated CH
2IOO
# and O
2.
Keywords:
iodine atom; Criegee intermediate; yield; oxygen; collision efficiency