Abstract
A useful, compound-dependent gas/particle partition coefficient in the atmosphere is K p =(F/TSP)/A where F (ng/m 3 ) and A (ng/m 3 ) are the particle-associated and gaseous concentrations, and TSP (μg/m 3 ) is the total suspended particulate matter concentration. K p depends on temperature (T, K) according to log K p =m p /T+b p . Using urban field data from Osaka, Japan, the effects of relative humidity (RH, %) on measured k p values are examined over the range 42%≤relative humidity≤95%
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
