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Scientific Articles - PTR-MS Bibliography

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Found 4 results
Title [ Year(Asc)]
Filters: Author is Joó, E  [Clear All Filters]
[Simpraga2013] Šimpraga, M., H. Verbeeck, J. Bloemen, L. Vanhaecke, M. Demarcke, E. Joó, O. Pokorska, C. Amelynck, N. Schoon, J. Dewulf, et al., "Vertical canopy gradient in photosynthesis and monoterpenoid emissions: An insight into the chemistry and physiology behind", Atmospheric Environment: Elsevier, 2013.
It is well known that vertical canopy gradients and varying sky conditions influence photosynthesis (Pn), specific leaf area (SLA), leaf thickness (LT) and leaf pigments (lutein, â-carotene and chlorophyll). In contrast, little is known about these effects on monoterpenoid (MT) emissions. Our study examines simultaneously measured Pn, MT emissions and the MT/Pn ratio along the canopy of an adult European beech tree (Fagus sylvatica L.) in natural forest conditions. Dynamic branch enclosure systems were used at four heights in the canopy (7, 14, 21 and 25 m) in order to establish relationships and better understand the interaction between Pn and MT emissions under both sunny and cloudy sky conditions. Clear differences in Pn, MT emissions and the MT/Pn ratio were detected within the canopy. The highest Pn rates were observed in the sun leaves at 25 m due to the higher intercepted light levels, whereas MT emissions (and the MT/Pn ratio) were unexpectedly highest in the semi-shaded leaves at 21 m. The higher Pn rates and, apparently contradictory, lower MT emissions in the sun leaves may be explained by the hypothesis of Owen and Peñuelas (2005), stating synthesis of more photo-protective carotenoids may decrease the emissions of volatile isoprenoids (including MTs) because they both share the same biochemical precursors. In addition, leaf traits like SLA, LT and leaf pigments clearly differed with height in the canopy, suggesting that the leaf's physiological status cannot be neglected in future research on biogenic volatile organic compounds (BVOCs) when aiming at developing new and/or improved emission algorithms.
[Laffineur2011] Laffineur, Q., B. Heinesch, N. Schoon, C. Amelynck, J-F. Müller, J. Dewulf, H. Van Langenhove, E. Joó, K. Steppe, and M. Aubinet, "What can we learn from year-round BVOC disjunct eddycovariance measurements? A case example from a temperate forest", 5th International PTR-MS Conference on Proton Transfer Reaction Mass Spectrometry and its Applications: Innsbruck university press, 2011.
[Demarcke2010] Demarcke, M., J-F. Müller, N. Schoon, H. Van Langenhove, J. Dewulf, E. Joó, K. Steppe, M. Šimpraga, B. Heinesch, M. Aubinet, et al., "History effect of light and temperature on monoterpenoid emissions from Fagus sylvatica L.", Atmospheric Environment, vol. 44, no. 27: Elsevier, pp. 3261–3268, 2010.
Monoterpenoid emissions from Fagus sylvatica L. trees have been measured at light- and temperature-controlled conditions in a growth chamber, using Proton Transfer Reaction Mass Spectrometry (PTR-MS) and the dynamic branch enclosure technique. De novo synthesized monoterpenoid Standard Emission Factors, obtained by applying the G97 algorithm (Guenther, 1997), varied between 2 and 32 μg gDW−1 h−1 and showed a strong decline in late August and September, probably due to senescence. The response of monoterpenoid emissions to temperature variations at a constant daily light pattern could be well reproduced with a modified version of the MEGAN algorithm (Guenther et al., 2006), with a typical dependence on the average temperature over the past five days. The diurnal emissions at constant temperature showed a typical hysteretic behaviour, which could also be adequately described with the modified MEGAN algorithm by taking into account a dependence on the average light levels experienced by the trees during the past 10–13 h. The impact of the past light and temperature conditions on the monoterpenoid emissions from F. sylvatica L. was found to be much stronger than assumed in previous algorithms. Since our experiments were conducted under low light intensity, future studies should aim at confirming and completing the proposed algorithm updates in sunny conditions and natural environments.
[Steppe2009] Steppe, K., R. Lemeur-UGent, J. Dewulf, H. Van Langenhove-UGent, C. Amelynck, N. Schoon, J-F. Müller-BISA, M. Aubinet-FUSAG, J. Dewulf, E. Joó, et al., "IMPACT OF PHENOLOGY AND ENVIRONMENTAL CONDITIONS ON BVOC EMISSIONS FROM FOREST ECOSYSTEMS IMPECVOC", Science for Sustainable Development (SSD), 2009.

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Selected PTR-MS related Reviews

F. Biasioli, C. Yeretzian, F. Gasperi, T. D. Märk: PTR-MS monitoring of VOCs and BVOCs in food science and technology, Trends in Analytical Chemistry 30 (7) (2011).

J. de Gouw, C. Warneke, T. Karl, G. Eerdekens, C. van der Veen, R. Fall: Measurement of Volatile Organic Compounds in the Earth's Atmosphere using Proton-Transfer-Reaction Mass Spectrometry. Mass Spectrometry Reviews, 26 (2007), 223-257.

W. Lindinger, A. Hansel, A. Jordan: Proton-transfer-reaction mass spectrometry (PTR–MS): on-line monitoring of volatile organic compounds at pptv levels, Chem. Soc. Rev. 27 (1998), 347-375.


Lists with PTR-MS relevant publications of the University of Innsbruck can be found here: Atmospheric and indoor air chemistry, IMR, Environmental Physics and Nano-Bio-Physics


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