Author/Authors :
By THOMAS CUSTER ، نويسنده , , GUNNAR SCHADE، نويسنده ,
Abstract :
Oxygenated volatile organic compounds (OVOCs) play an active role in tropospheric chemistry but our knowledge
concerning their release and ultimate fate is limited. However, the recent introduction of Proton Transfer Reaction Mass
Spectrometry (PTRMS) has improved our capability to make direct field observations ofOVOC mixing ratios and fluxes.
We used PTRMS in an eddy covariance setup to measure selected OVOC exchange rates above a well-characterized
agricultural plot in Northern Germany. In fall 2003, mixing ratios of methanol and acetaldehyde 2mabove the field ranged
from 1 to 10 and 0.4 to 2.1 ppb, respectively, well correlated with one another. Fluxes of both gases were followed for
growing Italian ryegrass (Lolium multiflorum) over a significant portion of its life cycle. Diurnally fluctuating emissions
of methanol and very small acetaldehyde fluxes were observed up to the cutting and removal of the grass. Methanol
emissions were exponentially related to ambient temperatures and appeared to be higher during the grass’ rapid leaf
area expansion and after a rain event. Acetaldehyde exchanges averaged over the whole period indicated very slow
deposition. Our measurements confirm previous, similar results, as well as presumptions that grasses are comparatively
low methanol emitters compared to non-grass species