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000049559 084__ $$2WoS$$aEcology
000049559 084__ $$2WoS$$aGeosciences, Multidisciplinary
000049559 1001_ $$0P:(DE-HGF)0$$aSandoval-Soto, J. S. K.$$b0
000049559 245__ $$aGlobal uptake of carbonyl sulfide (COS) by terrestrial vegetation: Estimates corrected by deposition velocities normalized to the uptake of carbon dioxide (CO2)
000049559 260__ $$aKatlenburg-Lindau [u.a.]$$bCopernicus$$c2005
000049559 300__ $$a125 - 132
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000049559 520__ $$aCOS uptake by trees, as observed under dark/light changes and under application of the plant hormone abscisic acid, exhibited a strong correlation with the CO2 assimilation rate and the stomatal conductance. As the uptake of COS occurred exclusively through the stomata we compared experimentally derived and re-evaluated deposition velocities (V-d; related to stomatal conductance) for COS and CO2. We show that Vd of COS is generally significantly larger than that of CO2. We therefore introduced this attribute into a new global estimate of COS fluxes into vegetation. The new global estimate of the COS uptake based on available net primary productivity data (NPP) ranges between 0.69-1.40 Tg a(-1). However, as a COS molecule is irreversibly split in contrast to CO2 which is released again by respiration processes, we took into account the Gross Primary Productivity (GPP) representing the true CO2 leaf flux the COS uptake has to be related to. Such a GPP based deposition estimate ranged between 1.4-2.8 Tg a(-1) (0.73-1.50 Tg S a(-1)). We believe that in order to obtain accurate global COS sink estimates such a GPP-based estimate corrected by the different deposition velocities of COS and CO2 must be taken into account.
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000049559 7001_ $$0P:(DE-HGF)0$$aStanimirov, M.$$b1
000049559 7001_ $$0P:(DE-Juel1)VDB14301$$avon Hobe, M.$$b2$$uFZJ
000049559 7001_ $$0P:(DE-HGF)0$$aSchmitt, V.$$b3
000049559 7001_ $$0P:(DE-HGF)0$$aValdes, J.$$b4
000049559 7001_ $$0P:(DE-HGF)0$$aWild, A.$$b5
000049559 7001_ $$0P:(DE-HGF)0$$aKesselmeier, J.$$b6
000049559 773__ $$0PERI:(DE-600)2158181-2$$gVol. 2, p. 125 - 132$$p125 - 132$$q2<125 - 132$$tBiogeosciences$$v2$$x1726-4170$$y2005
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