The HO-Br bond energy (and consequently the heat of formation of HOBr) has been determined experimentally for the first time. HOBr can be photolyzed in the stratosphere to form Br and OH, both of which can react with ozone, and destroy it. Previous calculations modeling stratospheric reactions have assumed a lower stability than that found in the current research. The stability of HOBr was determined by measuring the threshold for formation of Br{sup +} from this molecule, using photoionization mass spectrometry. Their work was supported by the Division of Chemical Sciences, Office of Basic Energy Sciences
The reaction BrO + HO_2 → products is the rate-limiting step in a key catalytic ozone destruction cy...
The impact of new laboratory data for the reaction BrO + HO2 yields HOBr + O2 in the depletion of gl...
The HOO radical is a key intermediate in the atmosphere and is involved in a large number of reactio...
International audienceThe impact of new laboratory data for the reaction BrO + HO2-> HOBr + 02 has b...
Short communicationInternational audienceIn the mid 1980s the study of ozone reactivity gained a sig...
Abstract. We have used a constrained one-dimensional photochemical model to investigate the effect o...
Over the last two decades it has emerged that measured hydroxyl radical levels in the upper troposph...
Over the last two decades it has emerged that measured hydroxyl radical levels in the upper troposph...
The HOBr molecule is a potential reservoir of Br compounds in the atmosphere. In this work, the UV-...
Abstract. This paper considers the effect of heterogeneous bromine reactions on stratospheric photoc...
A theoretical study has been made of the BrO + HO2 reaction, a radical–radical reaction which contri...
Hydrogen bromide (HBr) is the principal bromine sink species for the ozone loss chemistry induced by...
In this work, feasible mechanisms and pathways of the C2H5O2 + BrO reaction in the atmosphere were i...
We determine mixing ratio profiles for HBr and upper limits for HOBr in the stratosphere with precis...
The ozone depletion potential (ODP) of methyl bromide (CH_3Br) can be determined by combining the mo...
The reaction BrO + HO_2 → products is the rate-limiting step in a key catalytic ozone destruction cy...
The impact of new laboratory data for the reaction BrO + HO2 yields HOBr + O2 in the depletion of gl...
The HOO radical is a key intermediate in the atmosphere and is involved in a large number of reactio...
International audienceThe impact of new laboratory data for the reaction BrO + HO2-> HOBr + 02 has b...
Short communicationInternational audienceIn the mid 1980s the study of ozone reactivity gained a sig...
Abstract. We have used a constrained one-dimensional photochemical model to investigate the effect o...
Over the last two decades it has emerged that measured hydroxyl radical levels in the upper troposph...
Over the last two decades it has emerged that measured hydroxyl radical levels in the upper troposph...
The HOBr molecule is a potential reservoir of Br compounds in the atmosphere. In this work, the UV-...
Abstract. This paper considers the effect of heterogeneous bromine reactions on stratospheric photoc...
A theoretical study has been made of the BrO + HO2 reaction, a radical–radical reaction which contri...
Hydrogen bromide (HBr) is the principal bromine sink species for the ozone loss chemistry induced by...
In this work, feasible mechanisms and pathways of the C2H5O2 + BrO reaction in the atmosphere were i...
We determine mixing ratio profiles for HBr and upper limits for HOBr in the stratosphere with precis...
The ozone depletion potential (ODP) of methyl bromide (CH_3Br) can be determined by combining the mo...
The reaction BrO + HO_2 → products is the rate-limiting step in a key catalytic ozone destruction cy...
The impact of new laboratory data for the reaction BrO + HO2 yields HOBr + O2 in the depletion of gl...
The HOO radical is a key intermediate in the atmosphere and is involved in a large number of reactio...