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Seasonal differences in isoprene and light-dependent monoterpene emission by Amazonian tree species [Review]

机译:亚马逊树种异戊二烯和光依赖性单萜的季节变化[综述]

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Whereas for extra-tropical regions model estimates of the emission of volatile organic compounds (VOC) predict strong responses to the strong annual cycles of foliar biomass, light intensity and temperature, the tropical regions stand out as a dominant source year round, with only little variability mainly due to the annual cycle of foliar biomass of drought-deciduous trees. As part of the Large Scale Biosphere Atmosphere Experiment in Amazonia (LBA-EUSTACH), a remote secondary tropical forest site was visited in the dry-to-wet season transition campaign, and the trace gas exchange of a strong isoprene emitter and a monoterpene emitter are compared to the wet-to-dry season transition investigations reported earlier. Strong seasonal differences of the emission capacity were observed. The standard emission factor for isoprene emission of young mature leaves of Hymenaea courbaril was about twofold in the end of the dry season (111.5 mugC g(-1) h(-1) or 41.2 nmol m(-2) s(-1)) compared to old mature leaves investigated in the end of the wet season (45.4 mugC g(-1) h(-1) or 24.9 nmol m(-2) s(-1)). Standardized monoterpene emission rate of Apeiba tibourbou were 2.1 and 3.6 mugC g(-1) h(-1) (or 0.3 and 0.8 nmol m(-2) s(-1)), respectively. This change in species-specific VOC emission capacity was mirrored by a concurrent change in the ambient mixing ratios. The growth conditions vary less in tropical areas than in temperate regions of the world, and the seasonal differences in emission strength could not be reconciled solely with meteorological data of instantaneous light intensity and temperature. Hence the inadequacy of using a single standard emission factor to represent an entire seasonal cycle is apparent. Among a host of other potential factors, including the leaf developmental stage, water and nutrient status, and abiotic stresses like the oxidative capacity of the ambient air, predominantly the long-term growth temperature may be applied to predict the seasonal variability of the isoprene emission capacity. The dry season isoprene emission rates of H. courbaril measured at the canopy top were also compared to isoprene emissions of the shade-adapted species Sorocea guilleminiana growing in the understory. Despite the difference in VOC emission composition and canopy position, one common algorithm was able to predict the diel emission pattern of all three tree species.
机译:对于温带地区,挥发性有机化合物(VOC)排放量的模型估算值预测了对叶片生物量,光照强度和温度的强年周期的强烈响应,而热带地区则是全年的主要来源,而几乎没有变异主要是由于干旱落叶树的叶片生物量的年循环。作为亚马逊大生物圈大气实验(LBA-EUSTACH)的一部分,在从干湿过渡的过程中,参观了一个偏远的次生热带森林,并进行了强异戊二烯和单萜排放的微量气体交换。与之前报道的干湿过渡研究进行了比较。观察到排放能力的强烈季节性差异。在干燥季节结束时(111.5 mugC g(-1)h(-1)或41.2 nmol m(-2)s(-1),绣球花幼嫩叶的异戊二烯排放的标准排放因子约为两倍。 )与在雨季结束时调查的旧的成熟叶子相比(45.4 mugC g(-1)h(-1)或24.9 nmol m(-2)s(-1))。 Apeiba tibourbou的标准单萜排放速率分别为2.1和3.6 mugC g(-1)h(-1)(或0.3和0.8 nmol m(-2)s(-1))。特定物种的VOC排放量的这种变化反映了环境混合比的同时变化。热带地区的生长条件与世界温带地区相比变化较小,并且仅靠瞬时光强度和温度的气象数据无法解决发射强度的季节性差异。因此,使用单个标准排放因子来代表整个季节周期是不充分的。在许多其他潜在因素中,包括叶片发育阶段,水分和养分状况以及非生物胁迫(例如环境空气的氧化能力),主要是长期生长温度可用于预测异戊二烯排放的季节性变化容量。还比较了在树冠顶部测得的H. courbaril的干燥季节异戊二烯排放速率与生长在林下的适应阴暗的物种Sorocea guilleminiana的异戊二烯排放量。尽管VOC排放成分和树冠位置有所不同,但一种通用算法能够预测所有三种树种的diel排放模式。

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