The chemical lifetime of NOx in the boundary layer is approximately
— | 1 hour |
— | 20 hours |
— | 6 hours |
— | 36 hours |
The chemical lifetime of NOx in the upper troposphere is approximately
— | a few hours |
— | several days to a week |
— | a day |
— | a month |
The rapid breakdown of NOx leads to a large variation in its concentration. Urban areas can have concentrations in the order of
— | 10 parts per billion by volume |
— | 10 parts per million by volume |
— | 10 parts per thousand by volume |
— | 10 parts per trillion by volume |
whereas remote regions such as the upper troposphere and the boundary layers over remote areas of oceans can have concentrations in the order of
— | 10 parts per billion by volume. |
— | 10 parts per million by volume. |
— | 10 parts per thousand by volume. |
— | 10 parts per trillion by volume. |
The breakdown of NO2 can produce HNO3, which
— | permanently binds NOx. |
— | acts as a temporary reservoir for NOx. |
— | can itself be a source of NOx. |
— | is only produced during daylight. |
NB You can choose several options
During the day
— | HNO3 is rapidly photolysed. |
— | Reacts directly with CH4 or other hydrocarbons. |
— | HNO3 uses up NOx. |
HNO3 acts as a sink for NO2
— | more during the day. |
— | equally during night and day. |
— | more during the night. |