Interannual and seasonal changes in the soil exchange rates of monoterpenes andother VOCS in a Mediterranean shrubland

Abstract:

<p><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">Information about soil VOC inventories and exchange rates in different soils is very scarce. Seasonality of soil VOC exchange rates is also largely unknown, despite the increasing interest in some soil volatile compounds, such as monoterpenes, because of their important role in soil ecology. We aimed to explore and quantify soil VOC exchange rates in a Mediterranean shrubland and their seasonality. Measurements of soil VOC exchange were taken using GC-MS and PTR-MS techniques, together with soil temperature, soil moisture and soil CO</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">2<span style="font-size: small;"> </span></span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">efflux measurements, during two annual campaigns with contrasting precipitation. Methanol, acetic acid, ethyl acetate, acetaldehyde, acetone, C</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">3 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">and C</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">4 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">carbonyls (such as methyl ethyl ketone), </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">a</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">-pinene and limonene, showed the highest emission rates. Maximum soil monoterpene emission rates were very low (0.003 nmol m-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">2 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">s-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">1</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">) compared with foliar monoterpene emissionrates. The emission rates of the other VOCs were also low (maximum 0.8 nmol m</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">-2 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">s-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">1</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">) except for methanol (1.2 nmol m</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">2 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">s-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">1</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">). Maximum soil uptake rates for some VOCs, such as methanol and acetonitrile (ranging from </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">0.1 to -</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">0.5 nmol m-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">2 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">s-</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">1</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">) were, however, comparable with foliar uptakerates. Further studies are needed to corroborate these results and the possible importance of the soil VOC sink in regional chemistry-climate models. Long-term severe drought increased soil monoterpene emission rates in this Mediterranean shrubland. The increases seem to be linked to changes in the soil’s physical properties induced by low soil moisture. Unlike monoterpenes, other soil VOC emission rates decreased when soil moisture was low. The results suggest a seasonal control of soil temperature on the emission rates of monoterpenes and other VOCs. The emission rates increase with soil temperature. Positive correlations between the VOC exchange rates and the soil CO</span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">2 </span><span style="font-size: x-small; font-family: tahoma,arial,helvetica,sans-serif;">fluxes suggest that phenology of <span style="font-size: xx-small;">roots and microorganisms also controls seasonal changes in soil VOCs in this Mediterranean shrubland.</span></span></p>
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