Seasonal variation of mono- and sesquiterpene emission rates of Scots pine

被引:174
作者
Hakola, H
Tarvainen, V
Bäck, J
Ranta, H
Bonn, B
Rinne, J
Kulmala, M
机构
[1] Finnish Meteorol Inst, Air Chem Lab, Helsinki 00101, Finland
[2] Univ Helsinki, Dept Forest Ecol, Helsinki, Finland
[3] Univ Helsinki, Dept Phys Sci, Helsinki 00014, Finland
[4] Univ Turku, Dept Biol, Turku 20014, Finland
关键词
D O I
10.5194/bg-3-93-2006
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The seasonal variation of mono-and sesquiterpene emission rates of Scots pine was measured from April to October in 2004. The emission rates were measured daily in the afternoons with the exception of weekends. Emissions were measured from two branches; one of them was debudded in May (branch A), while the other was allowed to grow new needles (branch B). The monoterpene emission pattern remained almost constant throughout the measurement period, Delta(3)-carene being the dominant monoterpene (50-70% of the VOC emission). The standard monoterpene emission potential (30 degrees C) was highest during early summer in June (the average of the two branches 1.35 g g(-1) h(-1)) and lowest during early autumn in September (the average of the two branches 0.20 g g(-1) h(-1)). The monoterpene emission potential of branch A remained low also during October, whereas the emission potential of branch B was very high in October. The sesquiterpenes were mainly emitted during mid summer, the dominant sesquiterpene being beta-caryophyllene. Branch A had a higher sesquiterpene emission potential than branch B and the emission maximum occurred concomitant with the high concentration of airborne pathogen spores suggesting a potential defensive role of the sesquiterpene emissions. The sesquiterpene emissions were well correlated with linalool and 1,8-cineol emissions, but not with monoterpenes. Sesquiterpene and 1,8-cineol emissions were equally well described by the temperature dependent and the temperature and light dependent algorithms. This is due to the saturation of the light algorithm as the measurements were always conducted during high light conditions.
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页码:93 / 101
页数:9
相关论文
共 32 条
[1]   Sesquiterpene ozonolysis: Origin of atmospheric new particle formation from biogenic hydrocarbons [J].
Bonn, B ;
Moortgat, GK .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (11) :39-1
[2]   THE OBSERVATION OF A C5 ALCOHOL EMISSION IN A NORTH-AMERICAN PINE FOREST [J].
GOLDAN, PD ;
KUSTER, WC ;
FEHSENFELD, FC ;
MONTZKA, SA .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (11) :1039-1042
[3]  
Guenther A, 1997, ECOL APPL, V7, P34, DOI 10.1890/1051-0761(1997)007[0034:SASVIN]2.0.CO
[4]  
2
[5]   ISOPRENE AND MONOTERPENE EMISSION RATE VARIABILITY - MODEL EVALUATIONS AND SENSITIVITY ANALYSES [J].
GUENTHER, AB ;
ZIMMERMAN, PR ;
HARLEY, PC ;
MONSON, RK ;
FALL, R .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1993, 98 (D7) :12609-12617
[6]   The hydrocarbon emission rates of tea-leafed willow (Salix phylicifolia), silver birch (Betula pendula) and European aspen (Populus tremula) [J].
Hakola, H ;
Rinne, J ;
Laurila, T .
ATMOSPHERIC ENVIRONMENT, 1998, 32 (10) :1825-1833
[7]   Seasonal variation of VOC concentrations above a boreal coniferous forest [J].
Hakola, H ;
Tarvainen, V ;
Laurila, T ;
Hiltunen, V ;
Hellén, H ;
Keronen, P .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (12) :1623-1634
[8]  
Hakola H, 2001, BOREAL ENVIRON RES, V6, P237
[9]   The ambient concentrations of biogenic hydrocarbons at a northern European, boreal site [J].
Hakola, H ;
Laurila, T ;
Rinne, J ;
Puhto, K .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (29-30) :4971-4982
[10]   Emission of 2-methyl-3-buten-2-ol by pines: A potentially large natural source of reactive carbon to the atmosphere [J].
Harley, P ;
Fridd-Stroud, V ;
Greenberg, J ;
Guenther, A ;
Vasconcellos, P .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D19) :25479-25486