Isoprene and α-pinene deposition to grassland mesocosms
Background and aims Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by vegetation into the atmosphere. Previous research focussed on the magnitude of and controls on emissions of these two compounds by emitting plant s...
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| Published in | Plant and soil Vol. 410; no. 1/2; pp. 313 - 322 |
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| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Cham
Springer
01.01.2017
Springer International Publishing |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0032-079X 1573-5036 1573-5036 |
| DOI | 10.1007/s11104-016-3009-8 |
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| Abstract | Background and aims Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by vegetation into the atmosphere. Previous research focussed on the magnitude of and controls on emissions of these two compounds by emitting plant species, while the role of soils and non-emitting plant species as potential sinks has been mostly ignored. The objective of the present study is to characterize the deposition of isoprene and α-pinene (a monoterpene) to non-emitting grassland plant mesocosms. Methods We conducted a laboratory experiment with mesocosms of two forb and one graminoid plant species. Plants and soils together and bare soils only were subject to increasing ambient isoprene and α-pinene concentrations (0-10 ppbv) and the corresponding BVOC exchange rates were quantified. Results Our major findings are that (i) soils were the dominant sink for the deposition of α-pinene and isoprene in grassland mesocosms, (ii) the presence of above-ground biomass of non-emitting plant species decreased the isoprene and α-pinene deposition in the majority of all cases, and (iii) the net deposition correlated inversely with the ambient concentrations. Conclusions Our results call for a more in-depth analysis of soil BVOC exchange to better estimate the contribution of soils to the ecosystem-atmosphere BVOC exchange. |
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| AbstractList | Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by vegetation into the atmosphere. Previous research focussed on the magnitude of and controls on emissions of these two compounds by emitting plant species, while the role of soils and non-emitting plant species as potential sinks has been mostly ignored. The objective of the present study is to characterize the deposition of isoprene and alpha -pinene (a monoterpene) to non-emitting grassland plant mesocosms. We conducted a laboratory experiment with mesocosms of two forb and one graminoid plant species. Plants and soils together and bare soils only were subject to increasing ambient isoprene and alpha -pinene concentrations (0-10 ppbv) and the corresponding BVOC exchange rates were quantified. Our major findings are that (i) soils were the dominant sink for the deposition of alpha -pinene and isoprene in grassland mesocosms, (ii) the presence of above-ground biomass of non-emitting plant species decreased the isoprene and alpha -pinene deposition in the majority of all cases, and (iii) the net deposition correlated inversely with the ambient concentrations. Our results call for a more in-depth analysis of soil BVOC exchange to better estimate the contribution of soils to the ecosystem-atmosphere BVOC exchange. BACKGROUND AND AIMS: Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by vegetation into the atmosphere. Previous research focussed on the magnitude of and controls on emissions of these two compounds by emitting plant species, while the role of soils and non-emitting plant species as potential sinks has been mostly ignored. The objective of the present study is to characterize the deposition of isoprene and α-pinene (a monoterpene) to non-emitting grassland plant mesocosms. METHODS: We conducted a laboratory experiment with mesocosms of two forb and one graminoid plant species. Plants and soils together and bare soils only were subject to increasing ambient isoprene and α-pinene concentrations (0–10 ppbv) and the corresponding BVOC exchange rates were quantified. RESULTS: Our major findings are that (i) soils were the dominant sink for the deposition of α-pinene and isoprene in grassland mesocosms, (ii) the presence of above-ground biomass of non-emitting plant species decreased the isoprene and α-pinene deposition in the majority of all cases, and (iii) the net deposition correlated inversely with the ambient concentrations. CONCLUSIONS: Our results call for a more in-depth analysis of soil BVOC exchange to better estimate the contribution of soils to the ecosystem-atmosphere BVOC exchange. Background and aims Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by vegetation into the atmosphere. Previous research focussed on the magnitude of and controls on emissions of these two compounds by emitting plant species, while the role of soils and non-emitting plant species as potential sinks has been mostly ignored. The objective of the present study is to characterize the deposition of isoprene and α-pinene (a monoterpene) to non-emitting grassland plant mesocosms. Methods We conducted a laboratory experiment with mesocosms of two forb and one graminoid plant species. Plants and soils together and bare soils only were subject to increasing ambient isoprene and α-pinene concentrations (0–10 ppbv) and the corresponding BVOC exchange rates were quantified. Results Our major findings are that (i) soils were the dominant sink for the deposition of α-pinene and isoprene in grassland mesocosms, (ii) the presence of above-ground biomass of non-emitting plant species decreased the isoprene and α-pinene deposition in the majority of all cases, and (iii) the net deposition correlated inversely with the ambient concentrations. Conclusions Our results call for a more in-depth analysis of soil BVOC exchange to better estimate the contribution of soils to the ecosystem-atmosphere BVOC exchange. |
| Audience | Academic |
| Author | Hansel, Armin Schnitzler, Jörg-Peter Wohlfahrt, Georg Ghirardo, Andrea Spielmann, Felix M. Langebner, Stephan |
| Author_xml | – sequence: 1 givenname: Felix M. surname: Spielmann fullname: Spielmann, Felix M. – sequence: 2 givenname: Stephan surname: Langebner fullname: Langebner, Stephan – sequence: 3 givenname: Andrea surname: Ghirardo fullname: Ghirardo, Andrea – sequence: 4 givenname: Armin surname: Hansel fullname: Hansel, Armin – sequence: 5 givenname: Jörg-Peter surname: Schnitzler fullname: Schnitzler, Jörg-Peter – sequence: 6 givenname: Georg surname: Wohlfahrt fullname: Wohlfahrt, Georg |
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| Snippet | Background and aims Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by... Background and aims Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by... Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by vegetation into the... BACKGROUND AND AIMS: Isoprene and monoterpenes account for approximately two thirds of the biogenic volatile organic compounds (BVOC) emitted annually by... |
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| SubjectTerms | aboveground biomass alpha-pinene Biomedical and Life Sciences Closed ecological systems Ecology emissions Environmental aspects forbs graminoids Grasslands isoprene Life Sciences Mesocosms Observations Plant Physiology Plant Sciences Regular Article soil Soil Science & Conservation volatile organic compounds |
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| Title | Isoprene and α-pinene deposition to grassland mesocosms |
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