Decline of soil volatile organic compounds from a Mediterranean deciduous forest under a future drier climate
Abstract
BVOC forest soil emission rate decreased by 43% under long term amplified drought (after 10 years of summer rain exclusion).
• Forest soil respiration was a strong driver of soil BVOC emissions.
• Temperature was positively correlated to forest soil BVOC emissions following Tingey's model. • Forest soil BVOC followed a diurnal pattern with maximum emissions during central hours of the day.
• Forest soil was mainly a source of BVOC but it was a sink of isoprene.
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Legros et al., 2025, Decline of soil volatile organic compounds from a Mediterranean deciduous forest under a future drier climate.pdf (3.13 Mo)
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