Acetone, methanol, and other partially oxidized volatile organic emissions from dead plant matter by abiological processes: Significance for atmospheric HO(X) chemistry

218Citations
Citations of this article
104Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

In this paper, attention is called to the significance of abiological production of partially oxidized volatile organic carbons (POVOCs) from the decay of dead plant material Measured relative emission of acetone and methanol can be at least 10-4 and 3 - 5 x 10-4 g g-1 of decaying dry plant matter, respectively. If these results may be extrapolated, global annual emissions of 6-8 Tg of acetone and 18 - 40 Tg of methanol would result, adding strongly to the estimated total emissions of these compounds to the atmosphere. Because acetone and methanol, through OH and HO2 formation, play significant roles in the chemistry of the atmosphere, further research is strongly needed to quantify the emissions of acetone, methanol, and other POVOCs.

Cite

CITATION STYLE

APA

Warneke, C., Karl, T., Judmaier, H., Hansel, A., Jordan, A., Lindinger, W., & Crutzen, P. J. (1999). Acetone, methanol, and other partially oxidized volatile organic emissions from dead plant matter by abiological processes: Significance for atmospheric HO(X) chemistry. Global Biogeochemical Cycles, 13(1), 9–17. https://doi.org/10.1029/98GB02428

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free