Monoterpene Emission Rates Research Articles

Impact of meteorological conditions on the biogenic volatile organic compound (BVOC) emission rate from eastern Mediterranean vegetation under drought

Abstract. A comprehensive characterization of drought's impact on biogenic volatile organic compound (BVOC) emissions is essential for understanding atmospheric chemistry under global climate change, with implications for both air quality and climate model simulation. Currently, the effects of drought on BVOC emissions are not well characterized. Our study aims to test (i) whether instantaneous changes in meteorological conditions can serve as a better proxy for drought-related changes in BVOC emissions compared to the absolute values of the meteorological parameters, as indicated by previous BVOC mixing-ratio measurements and (ii) the impact of a plant under drought stress receiving a small amount of precipitation on BVOC emission rate, and on the manner in which the emission rate is influenced by meteorological parameters. To address these objectives, we conducted our study during the warm and dry summer conditions of the eastern Mediterranean region, focusing on the impact of drought on BVOC emissions from natural vegetation. Specifically, we conducted branch-enclosure sampling measurements in Ramat Hanadiv Nature Park, under natural drought and after irrigation (equivalent to 5.5–7 mm precipitation) for six selected branches of Phillyrea latifolia, the highest BVOC emitter in this park, in September–October 2020. The samplings were followed by gas chromatography–mass spectrometry analysis for BVOC identification and flux quantification. The results corroborate the finding that instantaneous changes in meteorological parameters, particularly relative humidity (RH), offer the most accurate proxy for BVOC emission rates under drought compared to the absolute values of either temperature (T) or RH. However, after irrigation, the correlation of the detected BVOC emission rate with the instantaneous changes in RH became significantly more moderate or even reversed. Our findings highlight that under drought, the instantaneous changes in RH and to a lesser extent in T are the best proxy for the emission rate of monoterpenes (MTs) and sesquiterpenes (SQTs), whereas under moderate drought conditions, T or RH serves as the best proxy for MT and SQT emission rate, respectively. In addition, the detected emission rates of MTs and SQTs increased by 150 % and 545 %, respectively, after a small amount of irrigation.

Quantifying variabilities in monoterpene emission among natural individuals of an urban-greening species (Quercus phylliraeoides) using a rapid measuring method

Quercus phillyraeoides, a strong monoterpene-emitting species, is widely planted in urban and suburban areas in Japan. Urban-greening plants with terpenoid emission may affect air quality by increasing photochemical oxidants through the reaction between their terpenoid emissions and urban gases. In mitigating this issue, replacing the original plants with low-emitting variants can be a workable approach without substantially altering the original landscapes and ecotopes. This study aimed to identify the low- or non-emitting variants among Q. phillyraeoides. To deal with a large number of Q. phillyraeoides samples, a method using detached leaves was adopted and optimized for observation of terpenoid emission rates from Q. phillyraeoides. The testing showed that the emission rate would be relatively stable at approximately 40 min of incubation under a photosynthetic photon flux density of ∼1000 μmol m–2 s–1 and a surrounding temperature of 30°C. Although the emission rates were different from those derived using the conventional method (i.e., the leaf cuvette method), they were well calibrated, with a regression line between the datasets of the two methods. We used this method to inspect the monoterpene emission rate from Q. phillyraeoides in multiple locations in Shizuoka Prefecture and detected a variability in the monoterpene emission rate (no detection to 14.8 nmol m–2 s–1), which were independent of environmental effects for each location. The Q. phillyraeoides individuals with no emission of monoterpenes are expected to be suitable for propagation as non-terpenoid-emitting greening materials.

Emission of Terpenoid Compounds from Rice Plants

The global cultivation area of rice is equivalent to 4% of the world’s forest area and may be an important sink and source of trace gases. To produce a precise terpenoid emission inventory, it is essential to obtain reliable data of terpenoid emission from rice plants. In the present study, terpenoid emissions from various rice species were measured using flow-through chamber and tower flux measurement methods. In the flow-through chamber measurement, linalool was emitted from the above-ground parts of the three rice cultivars “Koshihikari”, “Nipponbare” and “IR72”. The emission rates gradually decreased (<0.1 µg gDW−1 h−1) within two days during the measurement periods. As the touching stimulus might have enhanced linalool emission, a non-contact measurement method, i.e., the tower flux measurement method, was applied to a “Koshihikari” paddy. Linalool was not detected, but α-pinene was detected in the atmosphere above the rice paddy. The α-pinene flux (mean ± 95% confidence interval) was 0.006 ± 0.004 nmol m−2 s−1 on a land-area basis. The flux was 1/200 of the previously reported monoterpene emission rate of the rice plants measured in a commercial chamber, but was not largely different from three other reports. We provide terpenoid flux data above a rice paddy for the first time, which is more reliable because the tower flux measurement method can avoid stimuli to rice leaves and stems. Although the obtained terpenoid emission rate is very low, the obtained values can contribute to the establishment of a precise BVOC inventory in Asia.

Indoor monoterpene emission rates from commercial cannabis cultivation facilities in Colorado

ABSTRACT In 2019, an air emissions field sampling study was conducted by the Colorado Department of Public Health and Environment’s Air Pollution Control Division (APCD) at four commercial cannabis cultivation facilities. Measurements of ambient biogenic volatile organic compounds (VOC) concentrations were collected from various growing stages of cannabis (vegetative and flowering) and during post-harvest activities (drying and trimming). These data were then used to determine room-specific biogenic VOC emission rates for three of the facilities from the vegetative stage of the life cycle through post-harvest activities. This study shows that the magnitude of biogenic VOC emissions within a cannabis cultivation facility varies widely with the highest emission rates of up to 7.18E–1 kg/hr found during mechanical trimming and up to 2.33E–1 kg/hr in the drying rooms. These were up to an order of magnitude higher than emission rates found in the cultivation rooms. For example, Facility A vegetative room had an emissions rate of 1.46E–2 kg/hr. Normalized by the amount of biomass present, the drying rooms had the highest VOC emissions rates, with a maximum rate of 1.6E–3 kg/hr/kg biomass. The flowering room rates were found to be up to 3.25E–4 kg/hr/kg biomass and drying rooms up to 1.16E–3 kg/hr/kg biomass. When normalized by plant count, emission rates in the flower rooms ranged from 8.11E–6 to 3.62E–4 kg/hr/plant. The dominant monoterpenes from sampling were β-myrcene, terpinolene, and D-limonene. These data suggest that the variability in emission rates across cannabis production will create a challenge in establishing a generalized emission factor for all facilities. Across the industry, cannabis cultivation conditions and strategies can vary widely impacting the amount and type of VOC emissions. Minimizing uncertainties for VOC emission from cannabis facilities requires site-specific information on air exchange rates, plant counts, cannabis strains, biomass, and if hand or mechanical processing is used. Implications: This study found that the magnitude of biogenic VOC emissions within a cannabis cultivation varies widely throughout rooms found in the facility, with the highest emissions found during post-harvest activities (i.e. trimming) and the lowest rates in the vegetative room. These data suggest that the large emission sources of VOCs are found post-harvest and emission inventories based solely on cultivation emissions will underestimate total biogenic VOC emissions from indoor cannabis cultivation facilities. The dominant measured terpenes throughout all facilities from cultivation to post harvest were: β-myrcene, terpinolene, and D-limonene.

城市植物挥发性有机化合物排放与臭氧相互作用及其机制

PDF HTML阅读 XML下载 导出引用 引用提醒 城市植物挥发性有机化合物排放与臭氧相互作用及其机制 DOI: 10.5846/stxb202202240431 作者: 作者单位: 作者简介: 通讯作者: 中图分类号: 基金项目: 长株潭城乡融合发展的生态环境效应与耦合机制项目（U21A2010） The interactions and mechanisms between biogenic volatile organic compounds emissions and ozone concentrations in urban areas: A review Author: Affiliation: Fund Project: 摘要 | 图/表 | 访问统计 | 参考文献 | 相似文献 | 引证文献 | 资源附件 | 文章评论 摘要:近地面臭氧（O3）已成为继PM2.5后影响我国空气质量的一种重要二次污染物。随着氮氧化物浓度的持续下降和气候变暖的加剧，城市O3的形成对挥发性有机化合物的浓度更加敏感。近年来城市绿色空间显著增长，植物源挥发性有机化合物（BVOCs）排放和浓度逐年增加。针对BVOCs与近地面O3之间复杂的交互作用，从植物BVOCs的特性与作用出发，综述了不同因素尤其是O3浓度增加对树木生理状态及BVOCs排放速率的影响，定量分析了已有研究中O3对不同植物异戊二烯和单萜烯排放速率的影响，以及BVOCs对O3形成的贡献，总结了BVOCs与O3相互作用研究领域存在的不足。未来亟需加强的研究包括：（1）城市树种BVOCs排放因子的实测，建立物种的排放速率数据库，优化模型参数，提升精细尺度BVOCs排放量估算模型精度；（2）多种环境因子，比如污染物浓度、温湿度等对城市植物BVOCs排放的交互作用和综合影响的研究；（3）植物BVOCs对O3形成贡献的定量研究，及其对植物抗污染能力的影响，为城市建设中的树种选择及减轻城市O3污染提供理论依据和借鉴。 Abstract:In China, surface ozone (O3) has become a major secondary pollutant as the fine particulate pollution problem was largely addressed. As nitrogen oxide concentrations continue to decline and climate warming intensifies, urban ozone formation becomes more sensitive to VOC emissions. With the continuous increase of urban green space in recent years, the emissions of Biogenic Volatile Organic Compounds (BVOCs) have also increased, and thus played an increased role in ozone formation. This paper presented a comprehensive review of the interactions and mechanisms between BVOCs emissions and ozone concentrations in urban areas. We first reviewed the current states and trends in the response of plant physiological state and BVOCs emission rate to environmental stress, especially the elevated O3 concentration, with a particular emphasis on previous studies that focused on the effects of O3 on isoprene and monoterpene emission rates of various plans. We then summarized the role of BVOCs plays in O3 formation. Based on the review of the existing studies, we found a few knowledge gaps and identified several priorities for future research:(1) studies on quantifying the BVOCs emission rate of different urban tree species to build a more comprehensive database for BVOCs emission rate that can be used to optimize the parameters of BVOCs emissions models, and thereby to improve the precision of the fine-scale BVOCs emission estimation; (2) Exploring the interaction and comprehensive influence of various environmental factors on BVOCs emissions from urban plants, such as pollutant concentration, temperature, and humidity; (3) Quantifying the contribution of plant BVOCs to O3 formation and its effect on plant resistance to air pollution, which aims to provide a theoretical basis and reference for the selection of tree species for urban greening and the reduction of urban O3 pollution. 参考文献 相似文献 引证文献

Characteristics of biogenic volatile organic compounds emitted from major species of street trees and urban forests

Emission characteristics of biogenic volatile organic compounds (BVOCs) (such as isoprene and monoterpenes) emitted from major species of street trees and urban forests by variations in temperature and photosynthetically active radiation (PAR) were investigated. The isoprene and monoterpene emission rates from Prunus sargentii, Ginkgo biloba, Zelkova serrata and Taxus cuspidata were meager. In contrast, the isoprene and monoterpene emission rates from Metasequoia glyptostroboides were very high. In particular, the emission of α-pinene from Metasequoia glyptostroboides was over 10,000 times higher than that from Ginkgo biloba. The patterns of isoprene emissions from the four tree species except for Metasequoia glyptostroboides concerning temperature and PAR were difficult to determine because the emission rate is very low. However, monoterpene emissions from all five tree species were clearly affected by temperature and PAR. These results showed that the characteristics of isoprene and monoterpene emissions differed depending on the tree species. Regarding monoterpene composition, α-pinene (81.3%) accounts for the majority of total monoterpenes from Metasequoia glyptostroboides. This could be a critical consideration when planting trees in an urban forest because BVOC emissions (e.g., α-pinene) have been well known to affect ground-level ozone formation rate via photochemical reaction with NOX. Since Metasequoia glyptostroboides showed relatively high BVOC emissions, the use of this type of tree in an urban forest with relatively high nitrogen oxide emissions should be carefully considered.

Impact of heat stress on foliar biogenic volatile organic compound emission and gene expression in tomato (Solanum lycopersicum) seedlings

We present foliar biogenic volatile organic compound (BVOC) emission data from 24-h heat-stressed tomato (Solanum lycopersicum) seedlings including speciated monoterpenes and sesquiterpenes and high time-resolution measurements of methyl salicylate and total monoterpenes. The median total monoterpene and total sesquiterpene emission rates at 30°C were 18.5 and 0.172 pmol m–2 s–1, respectively, which falls within the negligible emission category of previous studies. However, initial heat exposure (39°C or 42°C) increased the emissions of approximately half of the targeted compounds beyond what was predicted by current BVOC emission temperature response algorithms. The enhanced emissions were not always sustained for the entire duration of the heat stress and some plants exhibited a delayed monoterpene response, where emissions peaked toward the end of the heat treatment. Methyl salicylate, a known stress marker, responded differently to the heat stress than most of the other compounds. Heat stress increased methyl salicylate emissions in some plants (at least initially), but in others, emissions declined or did not change significantly. There was no significant correlation between the magnitude of gene expression and emission induction of monoterpenes or methyl salicylate. Furthermore, the emitted monoterpenes did not exhibit any apparent light-dependent behavior, which suggests that these monoterpene stress emissions mostly originated from light-independent foliar storage pools and not from increased de novo production. In contrast, methyl salicylate emissions appear to have contributions from both de novo synthesis and stored pools, as they showed both enzyme-controlled (i.e., light-dependent) and light-independent behaviors. Analyses of the foliar essential oils demonstrate that most of the emitted BVOCs were also present in stored pools. The pool sizes were generally large enough to sustain unstressed emission levels for days to months, and even years for some compounds. However, heat-induced emission enhancement can diminish the pool sizes of some BVOCs, which could decrease subsequent emissions.

Influence of increased nutrient availability on biogenic volatile organic compound (BVOC) emissions and leaf anatomy of subarctic dwarf shrubs under climate warming and increased cloudiness.

Background and AimsClimate change is subjecting subarctic ecosystems to elevated temperature, increased nutrient availability and reduced light availability (due to increasing cloud cover). This may affect subarctic vegetation by altering the emissions of biogenic volatile organic compounds (BVOCs) and leaf anatomy. We investigated the effects of increased nutrient availability on BVOC emissions and leaf anatomy of three subarctic dwarf shrub species, Empetrum hermaphroditum, Cassiope tetragona and Betula nana, and if increased nutrient availability modifies the responses to warming and shading.MethodsMeasurements of BVOCs were performed in situ in long-term field experiments in the Subarctic using a dynamic enclosure system and collection of BVOCs into adsorbent cartridges analysed by gas chromatography–mass spectrometry. Leaf anatomy was studied using light microscopy and scanning electron microscopy.Key ResultsIncreased nutrient availability increased monoterpene emission rates and altered the emission profile of B. nana, and increased sesquiterpene and oxygenated monoterpene emissions of C. tetragona. Increased nutrient availability increased leaf tissue thicknesses of B. nana and C. tetragona, while it caused thinner epidermis and the highest fraction of functional (intact) glandular trichomes for E. hermaphroditum. Increased nutrient availability and warming synergistically increased mesophyll intercellular space of B. nana and glandular trichome density of C. tetragona, while treatments combining increased nutrient availability and shading had an opposite effect in C. tetragona.ConclusionsIncreased nutrient availability may enhance the protection capacity against biotic and abiotic stresses (especially heat and drought) in subarctic shrubs under future warming conditions as opposed to increased cloudiness, which could lead to decreased resistance. The study emphasizes the importance of changes in nutrient availability in the Subarctic, which can interact with climate warming and increased cloudiness effects.

Drought effects on volatile organic compound emissions from Scots pine stems.

Tree stems have been identified as sources of volatile organic compounds (VOCs) that play important roles in tree defence and atmospheric chemistry. Yet, we lack understanding on the magnitude and environmental drivers of stem VOC emissions in various forest ecosystems. Due to the increasing importance of extreme drought, we studied drought effects on the VOC emissions from mature Scots pine (Pinus sylvestris L.) stems. We measured monoterpenes, acetone, acetaldehyde and methanol emissions with custom-made stem chambers, online PTR-MS and adsorbent sampling in a drought-prone forest over the hot-dry summer of 2018 and compared the emission rates and dynamics between trees in naturally dry conditions and under long-term irrigation (drought release). The pine stems were significant monoterpene sources. The stem monoterpene emissions potentially originated from resin, based on their similar monoterpene spectra. The emission dynamics of all VOCs followed temperature at a daily scale, but monoterpene and acetaldehyde emission rates decreased nonlinearly with drought over the summer. Despite the dry conditions, large peaks of monoterpene, acetaldehyde and acetone emissions occurred in late summer potentially due to abiotic or biotic stressors. Our results highlight the potential importance of stem emissions in the ecosystem VOC budget, encouraging further studies in diverse environments.

Impact of pyruvic acid photolysis on acetaldehyde and peroxy radical formation in the boreal forest: theoretical calculations and model results

Abstract. Based on the first measurements of gas-phase pyruvic acid (CH3C(O)C(O)OH) in the boreal forest, we derive effective emission rates of pyruvic acid and compare them with monoterpene emission rates over the diel cycle. Using a data-constrained box model, we determine the impact of pyruvic acid photolysis on the formation of acetaldehyde (CH3CHO) and the peroxy radicals CH3C(O)O2 and HO2 during an autumn campaign in the boreal forest. The results are dependent on the quantum yield (φ) and mechanism of the photodissociation of pyruvic acid and the fate of a likely major product, methylhydroxy carbene (CH3COH). With the box model, we investigate two different scenarios in which we follow the present IUPAC (IUPAC Task Group on Atmospheric Chemical Kinetic Data Evaluation, 2021) recommendations with φ = 0.2 (at 1 bar of air), and the main photolysis products (60 %) are acetaldehyde + CO2 with 35 % C–C bond fission to form HOCO and CH3CO (scenario A). In the second scenario (B), the formation of vibrationally hot CH3COH (and CO2) represents the main dissociation pathway at longer wavelengths (∼ 75 %) with a ∼ 25 % contribution from C–C bond fission to form HOCO and CH3CO (at shorter wavelengths). In scenario 2 we vary φ between 0.2 and 1 and, based on the results of our theoretical calculations, allow the thermalized CH3COH to react with O2 (forming peroxy radicals) and to undergo acid-catalysed isomerization to CH3CHO. When constraining the pyruvic acid to measured mixing ratios and independent of the model scenario, we find that the photolysis of pyruvic acid is the dominant source of CH3CHO with a contribution between ∼ 70 % and 90 % to the total production rate. We find that the photolysis of pyruvic acid is also a major source of the acetylperoxy radical, with contributions varying between ∼ 20 % and 60 % dependent on the choice of φ and the products formed. HO2 production rates are also enhanced, mainly via the formation of CH3O2. The elevated production rates of CH3C(O)O2 and HO2 and concentration of CH3CHO result in significant increases in the modelled mixing ratios of CH3C(O)OOH, CH3OOH, HCHO, and H2O2.

Seasonal emission of monoterpenes from four chemotypes of Cinnamomum camphora

Plant terpenes are the main functional agents in forest bathing and have great value in several industries. To uncover the seasonal variation of Cinnamomum camphora monoterpene emission and the difference among the chemotypes for promoting the development of forest bathing and exploitation of monoterpenes using the species, the emission of monoterpenes and related gene expression in the camphor chemotype, eucalyptol chemotype, linalool chemotype and borneol chemotype of C. camphora were analyzed in May (spring), July (summer) and November (autumn), and the stored monoterpenes and storage structure were investigated. Eleocytes were the storage structure of monoterpenes in C. camphora, which widely existed in the leaf palisade tissue and spongy tissue, as well as around the glands and vascular bundles. The 4 chemotypes of C. camphora released different monoterpene components which mainly derived from the immediate emission after synthesis. Camphor, eucalyptol, linalool and endo-borneol showed the uppermost emission rate and were the typical monoterpenes in the corresponding chemotype, respectively, due to the high expression of the genes encoding bornyl diphosphate synthase (E5.5.1.8), linalool synthase (TSP14) and (+)-neomenthol dehydrogenase (E1.1.1.208) for the biosynthesis of camphor, linalool and endo-borneol, respectively, and only expression of the gene encoding 1,8-cineole synthase (TSP-cin) for eucalyptol biosynthesis. Among the 4 chemotypes, the linalool chemotype showed the highest emission rate of monoterpenes in the same month (without significant difference with the eucalyptol chemotype in November), due to the high expression of the genes (dxs, dxr, ispF, gcpE, and GGPS) in methylerythritol-4-phosphate (MEP) pathway, α-terpineol synthase gene (E4.2.3.111) and TSP14. Among the 3 months, temperature was the remarkably varied meteorological condition. The highest monoterpene emission rate from the 4 chemotypes of C. camphora was detected in July, which should result from the up-regulated expression of related genes in monoterpene biosynthesis and improved vaporization and diffusion of stored monoterpenes under high temperature, with the former providing a major contribution.

Changes in light spectra modify secondary compound concentrations and BVOC emissions of Norway spruce seedlings

Our objective was to study how changes in the light spectra affect growth; the concentration of carbohydrate, chlorophyll, carotenoid, terpene, alkaloid, and phenolic compounds; and the emissions of BVOC (biogenic volatile organic compound) of Norway spruce (Picea abies (L.) Karst.) seedlings. This study was conducted during the growth of the third needle generation in plant growth chambers. The plants were exposed to two light spectra with equal photon flux densities but different proportions of blue light (400–500 nm) produced by LED (light-emitting diode) lamps: (i) control (white light + 12% blue light) and (ii) increased blue light (+B) (white light + 45% blue light). The +B treatment increased the concentrations of total flavonoids and acetophenones in needles. The major changes in the phenolic profile were an accumulation of astragalin derivatives and the aglycone of picein. The +B treatment also decreased concentrations of the main alkaloid compound, epidihydropinidine, and its precursor, 2-methyl-6-propyl-1,6-piperideine; the emission rates of limonene, myrcene, and total monoterpenes; and the concentrations of a few terpenoid compounds, mainly in stems. Growth as well as the carbohydrates and pigments present in the needles were not affected. The results suggest that supplemental blue light shifts carbon allocation between secondary metabolism routes — from alkaloid and terpenoid synthesis to flavonoid and acetophenone synthesis. The changes may affect herbivory and abiotic stress tolerance of Norway spruce.

Emissions of gaseous formic and acetic acids from major tree species in Japan

Gaseous formic and acetic acids are directly emitted from vegetation and produced by the photooxidation of biogenic volatile organic compounds in the atmosphere. Gaseous formic and acetic acid emissions from trees have not been well studied in Japan and the Asian region, and to gain further knowledge in this respect, we measured the emissions of formic and acetic acid emissions together with isoprene and monoterpene emissions from 10 major forest tree species and 10 major road tree species. All of the measured trees were found to emit gaseous formic and acetic acids from their leaves, but not all species emitted isoprene or monoterpene. The emission rates of formic (0.05–1.3 μg gDW−1 h−1) and acetic (0.10–1.43 μg gDW−1 h−1) acids were similar to those of some trees in Europe but higher than those of tropical tree species. No monthly variations were found in the emission rates of formic and acetic acids, but the emission rates of isoprene and monoterpene showed clear monthly variations. We calculated the ratio of direct emissions to direct plus secondary production derived by the photooxidation of formic and acetic acids by isoprene and monoterpene (direct/total emission ratio) relating to major forest and road tree species in Japan. For isoprene and monoterpene emitters, the average values of the direct/total emission ratio of formic and acetic acids in August were 62% (range: 9.0–88%) and 64% (range: 6.2–90%), respectively. The contribution degree of the direct/total emission ratio differed depending on the isoprene and monoterpene emission rates. The findings are suggestive of the importance of both direct emissions of gaseous formic and acetic acids from trees and the secondary formation of these acids via isoprene and monoterpene photooxidation. The present study may be useful for improving the estimation accuracy of formic and acetic acid emissions from vegetation in future climate change and air quality studies.

Differences in isoprene and monoterpene emissions from cold-tolerant eucalypt species grown in the UK

The UK may be required to expand its bioenergy production in order to make a significant contribution towards the delivery of its ‘net zero’ greenhouse gas emissions target by 2050. However, some trees grown for bioenergy are emitters of volatile organic compounds (VOCs), including isoprene and terpenes, precursors in the formation of tropospheric ozone, an atmospheric pollutant, which require assessment to understand any consequent impacts on air quality. In this initial scoping study, VOC emission rates were quantified under UK climate conditions for the first time from four species of eucalypts suitable for growing as short-rotation forest for bioenergy. An additional previously characterised eucalypt species was included for comparison. Measurements were undertaken using a dynamic chamber sampling system on 2-3 year-old trees grown under ambient conditions. Average emission rates for isoprene, normalised to 30 °C and 1000 μmol m−2 s−1 PAR, ranged between 1.3 μg C gdw−1 h−1 to 10 μg C gdw−1 h−1. All the eucalypt species measured were categorised as ‘medium’ isoprene emitters (1–10 μg C gdw−1 h−1). Total normalised monoterpene emission rates were of similar order of magnitude to isoprene or approximately one order of magnitude lower. The composition of the monoterpene emissions differed between the species and major compounds included eucalyptol, α-pinene, limonene and β-cis-ocimene. The emission rates presented here contribute the first data for further studies to quantify the potential impact on UK atmospheric composition, if there were widespread planting of eucalypts in the UK for bioenergy purposes.

Effect of growth temperature on monoterpene emission rates of Acer palmatum

To understand the effect of increasing atmospheric temperatures on monoterpene emissions from mature trees, we measured the monoterpene emission rate, monoterpene precursor content, and the SPAD value of Acer palmatum, a mature tree grown at three different field sites. The annual mean temperature differed by intervals of 3 °C among the three sites from 10.6 °C to 17.7 °C, depending on the site elevation. The short-term monoterpene emission rate of A. palmatum depended on both the leaf temperature and the light intensity. The growth temperature did not affect the monoterpene emissions in response to short-term variations in temperature and light intensity. The highest standard monoterpene emission rate, Ms, was observed from July to August, but this rate did not differ among the three sites. The Ms showed clear seasonal variation, whereas the monoterpene precursor content did not show them. The trend of the Ms was similar to that of the SPAD, as both values depend on leaf phenology. In A. palmatum, a warming of approximately 3 °C caused the start date of the monoterpene emissions to commence two to three weeks earlier, and end date of the monoterpene emissions to be delayed by two to three weeks. The cumulative temperature method could be used to predict the start and end dates of the monoterpene emissions. To estimate the annual monoterpene emissions, a temperature and light intensity dependent emission model was modified to incorporate the effect of growth temperature on seasonal patterns of Ms. Annual monoterpene emissions were found to increase linearly with annual mean temperature. For each 1 °C of warming, the annual monoterpene emissions from A. palmatum increased by approximately 15%. Our results suggest that the effect of growth temperature on monoterpene emissions should be considered when predicting monoterpene emissions in response to global warming in the foreseeable future.

Monoterpene emissions and the geranyl diphosphate content of Acer and Fagaceae species

ABSTRACT Monoterpenes emitted from trees play important roles in atmospheric chemistry through the formation of secondary organic aerosols and photochemical oxidants. Because monoterpene emissions from broad-leaved trees have rarely been studied in Japan, we measured the monoterpene emission rates of 20 Acer and 14 Fagaceae species. If a good correlation is found between the monoterpene precursor (geranyl diphosphate, GDP) content and monoterpene emission rate, the GDP content analysis in leaves may be an optional and simplified method to estimate monoterpene emission capacity of trees. To test this hypothesis, we investigated the relationship between GDP content in leaves and monoterpene emission rate of 13 tree species. Six Acer and 7 Fagaceae species were found to be monoterpene emitters. Although all of the measured trees contained GDP in their leaves, the presence or absence of monoterpene emissions was different for different species. Among the monoterpene emitters, no clear relationship was found between the basal emission rate (temperature: 30°C, photosynthetic photon flux density: 1000 μmol m−2 s−1) and GDP content. The ratio of the basal emission rate to GDP content differed between tree species. Our study demonstrated that the GDP content did not relate to the presence or absence of monoterpene production and its emission rate. We suggest that the activity or expression of monoterpene synthase may affect monoterpene emissions from Acer and Fagaceae species.

Sesquiterpenes dominate monoterpenes in northern wetland emissions

Abstract. We have studied biogenic volatile organic compound (BVOC) emissions and their ambient concentrations at a sub-Arctic wetland (Lompolojänkkä, Finland), which is an open, nutrient-rich sedge fen and a part of the Pallas-Sodankylä Global Atmosphere Watch (GAW) station. Measurements were conducted during the growing season in 2018 using an in situ thermal-desorption–gas-chromatograph–mass-spectrometer (TD-GC-MS). Earlier studies have shown that isoprene is emitted from boreal wetlands, and it also turned out to be the most abundant compound in the current study. Monoterpene (MT) emissions were generally less than 10 % of the isoprene emissions (mean isoprene emission over the growing season, 44 µg m−2 h−1), but sesquiterpene (SQT) emissions were higher than MT emissions all the time. The main MTs emitted were α-pinene, 1,8-cineol, myrcene, limonene and 3Δ-carene. Of SQTs cadinene, β-cadinene and α-farnesene had the major contribution. During early growing season the SQT∕MT emission rate ratio was ∼10, but it became smaller as summer proceeded, being only ∼3 in July. Isoprene, MT and SQT emissions were exponentially dependent on temperature (correlation coefficients (R2) 0.75, 0.66 and 0.52, respectively). Isoprene emission rates were also found to be exponentially correlated with the gross primary production of CO2 (R2=0.85 in July). Even with the higher emissions from the wetland, ambient air concentrations of isoprene were on average > 100, > 10 and > 6 times lower than MT concentrations in May, June and July, respectively. This indicates that wetland was not the only source affecting atmospheric concentrations at the site, but surrounding coniferous forests, which are high MT emitters, contribute as well. Daily mean MT concentrations had high negative exponential correlation (R2=0.96) with daily mean ozone concentrations indicating that vegetation emissions can be a significant chemical sink of ozone in this sub-Arctic area.

Emission patterns of biogenic volatile organic compounds from dominant forest species in Beijing, China

Biogenic volatile organic compounds (BVOCs) have significant effects on atmospheric chemistry, ozone formation and secondary organic aerosol formation. Considering few investigations about BOVCs emissions in north China where is facing serious air pollution in recent years, emissions of various BVOCs from 24 dominant forest species in Beijing were measured from June to September in 2018, using a dynamic headspace sampling method. More than one hundred BVOCs in the collected samples were identified by using an automatic thermal desorption-gas chromatography/mass spectrometry, and their emission rates based on leaf biomass were calculated. Isoprene and monoterpenes were verified to be the dominant BVOCs emitted from the tree species, accounting for more than 50% of the total BVOCs. Generally, broad-leaved species displayed high isoprene emission rates, especially the Platanus occidentalis (21.36 µg/(g⋅hr)), Robinia pseudoacacia (11.55 µg/(g⋅hr)), and Lonicera maackii (9.17 µg/(g⋅hr)), while coniferous species emitted high rates of monoterpenes, such as Platycladus orientalis (27.18 µg/(g⋅hr)), Pinus griffithii (23.11 µg/(g⋅hr)), and Pinus armandii (7.42 µg/(g⋅hr)). High emission rates of monoterpenes from the broad-leaved species of Buxus megistophylla (13.07 µg/(g⋅hr)) and Ligustrum vicaryi (5.74 µg/(g⋅hr)), and high isoprene emission rate from the coniferous tree of Taxus cuspidata (5.86 µg/(g⋅hr)) were also observed. The emission rates of sesquiterpenes from each tree were usually 10–100 times smaller than those of isoprene and monoterpenes. Additionally, relatively high emission rates of oxygenated volatile organic compounds and other alkenes than isoprene and monoterpenes were also found for several tree species.

Leaf isoprene and monoterpene emission distribution across hyperdominant tree genera in the Amazon basin

Tropical forests are acknowledged to be the largest global source of isoprene (C5H8) and monoterpenes (C10H16) emissions, with current synthesis studies suggesting few tropical species emit isoprenoids (20–38%) and do so with highly variable emission capacities, including within the same genera. This apparent lack of a clear phylogenetic thread has created difficulties both in linking isoprenoid function with evolution and for the development of accurate biosphere-atmosphere models. Here, we present a systematic emission study of “hyperdominant” tree species in the Amazon Basin. Across 162 individuals, distributed among 25 botanical families and 113 species, isoprenoid emissions were widespread among both early and late successional species (isoprene: 61.9% of the species; monoterpenes: 15.0%; both isoprene and monoterpenes: 9.7%). The hyperdominant species (69) across the top five most abundant genera, which make up about 50% of all individuals in the Basin, had a similar abundance of isoprenoid emitters (isoprene: 63.8%; monoterpenes: 17.4%; both 11.6%). Among the abundant genera, only Pouteria had a low frequency of isoprene emitting species (15.8% of 19 species). In contrast, Protium, Licania, Inga, and Eschweilera were rich in isoprene emitting species (83.3% of 12 species, 61.1% of 18 species, 100% of 8 species, and 100% of 12 species, respectively). Light response curves of individuals in each of the five genera showed light-dependent, photosynthesis-linked emission rates of isoprene and monoterpenes. Importantly, in every genus, we observed species with light-dependent isoprene emissions together with monoterpenes including β-ocimene. These observations support the emerging view of the evolution of isoprene synthases from β-ocimene synthases. Our results have important implications for understanding isoprenoid function-evolution relationships and the development of more accurate Earth System Models.

Biogenic volatile organic compound ambient mixing ratios and emission rates in the Alaskan Arctic tundra.

Rapid Arctic warming, a lengthening growing season, and the increasing abundance of biogenic volatile-organic-compound-emitting shrubs are all anticipated to increase atmospheric biogenic volatile organic compounds (BVOCs) in the Arctic atmosphere, with implications for atmospheric oxidation processes and climate feedbacks. Quantifying these changes requires an accurate understanding of the underlying processes driving BVOC emissions in the Arctic. While boreal ecosystems have been widely studied, little attention has been paid to Arctic tundra environments. Here, we report terpenoid (isoprene, monoterpenes, and sesquiterpenes) ambient mixing ratios and emission rates from key dominant vegetation species at Toolik Field Station (TFS; 68°38′ N, 149°36′ W) in northern Alaska during two back-to-back field campaigns (summers of 2018 and 2019) covering the entire growing season. Isoprene ambient mixing ratios observed at TFS fell within the range of values reported in the Eurasian taiga (0–500 parts per trillion by volume – pptv), while monoterpene and sesquiterpene ambient mixing ratios were respectively close to and below the instrumental quantification limit (~ 2 pptv). Isoprene surface emission rates ranged from 0.2 to 2250 μgC m−2 h−1 (mean of 85 μgC m−2 h−1) and monoterpene emission rates remained, on average, below 1 μgC m−2 h−1 over the course of the study. We further quantified the temperature dependence of isoprene emissions from local vegetation, including Salix spp. (a known isoprene emitter), and compared the results to predictions from the Model of Emissions of Gases and Aerosols from Nature version 2.1 (MEGAN2.1). Our observations suggest a 180 %–215 % emission increase in response to a 3–4°C warming, and the MEGAN2.1 temperature algorithm exhibits a close fit with observations for enclosure temperatures in the 0–30°C range. The data presented here provide a baseline for investigating future changes in the BVOC emission potential of the under-studied Arctic tundra environment.