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首页> 外文期刊>Biogeosciences >Global uptake of carbonyl sulfide (COS) by terrestrial vegetation: Estimates corrected by deposition velocities normalized to the uptake of carbon dioxide (COsub2/sub)
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Global uptake of carbonyl sulfide (COS) by terrestrial vegetation: Estimates corrected by deposition velocities normalized to the uptake of carbon dioxide (COsub2/sub)

机译:陆地植被对全球吸收的羰基硫(COS)的影响:通过归一化为二氧化碳吸收量(CO 2 )的沉积速度校正的估计值

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COS uptake by trees, as observed under dark/light changes and underapplication of the plant hormone abscisic acid, exhibited a strongcorrelation with the CO2 assimilation rate and the stomatalconductance. As the uptake of COS occurred exclusively through the stomatawe compared experimentally derived and re-evaluated deposition velocities(Vd; related to stomatal conductance) for COS and CO2. We show that Vd of COS is generallysignificantly larger than that of CO2. We therefore introduced thisattribute into a new global estimate of COS fluxes into vegetation. The newglobal estimate of the COS uptake based on available net primary productivitydata (NPP) ranges between 0.69-1.40 Tga-1. However, as a COS moleculeis irreversibly split in contrast to CO2 which is released again byrespiration processes, we took into account the Gross Primary Productivity(GPP) representing the true CO2 leaf flux the COS uptake has to berelated to. Such a GPP based deposition estimate ranged between 1.4-–2.8 Tga-1 (0.73-1.50 TgSa-1).We believe that in order to obtain accurate global COS sink estimates such a GPP-based estimate corrected bythe different deposition velocities of COS and CO2 must be taken into account.
机译:在黑暗/光亮变化和植物激素脱落酸施用不足的情况下,树木对COS的吸收与CO 2 同化率和气孔导度密切相关。由于COS的吸收仅通过气孔发生,因此比较了实验得出的和重新评估的COS和CO 2的沉积速度( V d ;与气孔导度有关) 。我们发现COS的 V d 通常显着大于CO 2 。因此,我们将此属性引入到COS入植被通量的全球新估算中。基于可用净初级生产力数据(NPP)的COS吸收量的新的全球估算范围为0.69-1.40 Tga -1 。但是,与通过呼吸过程再次释放的CO 2 相比,COS分子不可逆地分裂,因此我们考虑了代表真实CO 2 的总初级生产力(GPP) COS吸收与叶片通量有关。这种基于GPP的沉积估算值范围为1.4-–2.8 Tga -1 (0.73-1.50 TgSa -1 )。我们相信,为了获得准确的全球COS汇估算值必须考虑通过COS和CO 2 的不同沉积速度校正的基于GPP的估算。

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