z-logo
Premium
Automotive tire wear as a source for atmospheric OCS and CS 2
Author(s) -
Pos W. H.,
Berresheim H.
Publication year - 1993
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/93gl00972
Subject(s) - gas chromatography , atmosphere (unit) , ozone , mass spectrometry , sulfur , environmental science , nitrogen , flux (metallurgy) , environmental chemistry , analytical chemistry (journal) , materials science , chemistry , chromatography , metallurgy , meteorology , physics , organic chemistry
The emission of CS 2 , OCS and traces of SO 2 from mixtures of fifteen different ground tire treads has been detected in laboratory experiments using gas chromatography/flame photometric detection (GC/FPD) and gas chromatography/mass spectrometry (GC/MS). Samples of ground tire particles (60–100 mesh) were flushed at different temperatures using either clean nitrogen gas or a mixture of 100 ppb O 3 in N 2 . CS 2 was the dominant sulfur gas detected in all of the experiments. OCS and CS 2 emissions increased strongly with temperature and were independent of the presence of O 3 . In contrast, SO 2 was observed only at high ozone levels. It is roughly estimated that tire wear may produce as much as 0.04 ± 0.004 Tg S (OCS) yr −1 or about 6.7% of the total OCS flux into the atmosphere. Therefore, this as yet undescribed automotive source may make a small but significant contribution to the atmospheric OCS budget.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom