tures of J and/or limited maximum fraction of electrons used for isoprene synthesis. The model provides good fits to diurnal courses of field measurements of isoprene emission, and is also able to describe the changes in isoprene emission under stress conditions, for example, the decline in isoprene emission in water-stressed leaves.Key-words: atmospheric chemistry; emission modelling; isoprene emission; photosynthetic electron transport; volatile organic compounds.
INTRODUCTIONVolatile organic compounds (VOC) play an important role in ozone forming reactions in the troposphere (Liu et al. 1987;Chameides et al. 1988) as well as in determining accumulation rates of atmospheric greenhouse gases . At the global scale, biogenic emission of volatile organic compounds is estimated to be at least as large as, or larger than the anthropogenic emissions (Mueller 1992;Guenther et al. 1995). Yet the current estimates of biogenic emissions of VOC suffer from significant uncertainties, because of limited knowledge of physiological and environmental controls over VOC emission.Isoprene (2-methyl-1,3-butadiene) is the major emitted hydrocarbon in many species, and its emission is closely coupled to environmental conditions as well as to leaf physiological state. Current empirical algorithms employ an Arrhenius temperature relation of enzyme activity and a hyperbolic relationship with light to calculate the rates of isoprene emission in dependence upon leaf temperature and incident quantum flux density (Guenther, Monson & Fall 1991;Guenther et al. 1993;Geron, Guenther & Pierce 1994).Yet, within and between species, there is considerable variation in light and temperature responses observed in laboratory measurements of isoprene emission (Guenther et al. 1993;Harley, Guenther & Zimmerman 1996Lerdau & Keller 1997;Sharkey et al. 1999), and the empirical parameterizations are valid for very limited situations only. Present models also do not simulate the emission under stress conditions in a satisfactory manner, e.g.
ABSTRACTWe present a physiological model of isoprene (2-methyl-1,3-butadiene) emission which considers the cost for isoprene synthesis, and the production of reductive equivalents in reactions of photosynthetic electron transport for Liquidambar styraciflua L. and for North American and European deciduous temperate Quercus species. In the model, we differentiate between leaf morphology (leaf dry mass per area, M A , g m -2 ) altering the content of enzymes of isoprene synthesis pathway per unit leaf area, and biochemical potentials of average leaf cells determining their capacity for isoprene emission. Isoprene emission rate per unit leaf area (mmol m -2 s -1 ) is calculated as the product of M A , the fraction of total electron flow used for isoprene synthesis (e, mol mol -1 ), the rate of photosynthetic electron transport (J) per unit leaf dry mass (J m , mmol g -1 s -1 ), and the reciprocal of the electron cost of isoprene synthesis [mol isoprene (mol electrons -1 )]. The initial estimate of electron cost of isoprene...