Abstract

The emission of biogenic volatile organic compounds (BVOCs) is usually thought to depend on species-specific emission capacities that vary with seasonal and phenological conditions. Actual – so called constitutive - emissions are then calculated from prevailing temperature and radiation. However, various abiotic and biotic stressors such as ozone, extreme radiation and temperature conditions, as well as wounding e.g. from insect feeding, can lead to de-novo emissions of stress-induced BVOCs (sBVOCs) that may excel constitutive emissions by more than an order of magnitude. These emissions often have a considerable different compound composition and are short-lived but can prolong under continuous stress for quite some time. Thus they may easily have a large impact on overall regional BVOC emissions. However, sBVOCs are generally not considered in models since up to date no consistent mechanism has been suggested. This manuscript suggests a new mechanism based on the finding that sBVOCs originate from a handful of biosynthetic pathways which synthesize compounds in the groups of monoterpenes, sesquiterpenes, and green leave volatiles, as well as methyl salicylate, ethanol/acetaldehyde, methanol/formaldehyde, and acetone. Isoprene is also considered but since it is often constitutively emitted, the specific role of stress induction is difficult to determine for this compound. A function is proposed that describes the production of all de-novo sBVOCs sufficiently well and scales with stress intensity. It is hypothesized that the response delay and the form of the function is specific for the production pathway and valid for ozone as well as wounding (herbivory) induced stress. Model parameters are then derived from pooled literature data based on a meta-analysis of suitable induction-response measurements of different plant species. The overall emission amount then derives from the intensity and frequency of the stress impulse. We present a number of literature studies that are used to parameterize the new model as well as a selection of evaluations for single- and multiple-stress inductions. Furthermore, coupling and interaction with constitutive emission models as well as limitations and possible further developments are discussed.

Highlights

  • Volatile organic compounds (VOCs) are important precursors for the formation of tropospheric ozone and secondary aerosols (Shallcross and Monks, 2000; Atkinson and Arey, 2003)

  • biogenic volatile organic compounds (BVOCs) emissions have been studied since the late 1980’s and relationships between some main compounds and environmental conditions have been quantified for many plant species

  • It should be noted that parameters for enzyme kinetics (Td, α, μ) are not parameterized separately for each evaluation data set but are set independent from the plant species or the kind of stress

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Summary

Introduction

Volatile organic compounds (VOCs) are important precursors for the formation of tropospheric ozone and secondary aerosols (Shallcross and Monks, 2000; Atkinson and Arey, 2003). The new algorithm is applied on three independent data sets that either use ozone or herbivores as stressors over a defined time period so that simulated and measured emissions could be compared for different compound emissions over the course of several days.

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