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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Veröffentlicht in:Plant and soil 2017-01, Vol.410 (1/2), p.313-322
Hauptverfasser: Spielmann, Felix M., Langebner, Stephan, Ghirardo, Andrea, Hansel, Armin, Schnitzler, Jörg-Peter, Wohlfahrt, Georg
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container_end_page 322
container_issue 1/2
container_start_page 313
container_title Plant and soil
container_volume 410
creator Spielmann, Felix M.
Langebner, Stephan
Ghirardo, Andrea
Hansel, Armin
Schnitzler, Jörg-Peter
Wohlfahrt, Georg
description 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.
doi_str_mv 10.1007/s11104-016-3009-8
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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. 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source Jstor Complete Legacy; Springer Nature - Complete Springer Journals
subjects Biomedical and Life Sciences
Closed ecological systems
Ecology
Environmental aspects
Grasslands
Life Sciences
Mesocosms
Observations
Plant Physiology
Plant Sciences
Regular Article
Soil Science & Conservation
title Isoprene and α-pinene deposition to grassland mesocosms
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