T. Legros a, B. Temime-Roussel b, J. Kammer b, E. Quivet b, H. Wortham b, I.M. Reiter c, M. Santonja a, C. Fernandez a, E. Ormeño aaCNRS, Aix Marseille Univ, Avignon Univ, IRD, IMBE, Marseille, FrancebAix Marseille Univ, CNRS, LCE, Marseille, FrancecCNRS Fr3098 ECCOREV, 13545, Aix-en-Provence, France
Highlights
- Forest soil was mainly a source of BVOC but it was a sink of isoprene.
- 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
