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Geomorphology - key regulator of net methane and nitrous oxide fluxes from the pedosphere

机译:地貌学-来自对流层的甲烷和一氧化二氮净通量的关键调节器

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The scientific Global Change debate is hampered by the insufficient knowledge of "greenhouse gas" fluxes. Thereby, extrapolations of global warming potentials of soil derived trace gas fluxes arc sources of greatest uncertainties. At single ecosystems gas fluxes still show highly variable thus hardly predictable fluxes. Our main thesis was that geomorphology helps to explain much of the variability even at this detailed scale, i.e. under rather uniform ecological condition as seen from the surface. This thesis was tested at a site in Wildmooswald (Black Forest/SW-Germany) where recently soil individual fluxes were identified, but not the cause of the formation of such diverse and mainly hydromorphic pedosphere. The idea was that the periglacial slope deposits including a water-logging layer form a more complex relief than the present rather uniform relief. Thus explaining the diverging sod water and gas balances. The water-logging layer was mapped by a regular auger grid (25 X 20 m). The Global Warming Potential (CH4, N2O) was calculated by gas specific warming potential and area proportion of each soil type. Upper and lower relied were not congruent, thus the relief of periglacial slope deposits is explaining the spatial variability of N2O and CH4 emissions. The study field emitted 1,059 kg of CO2 equivalents ha a(-1) in average, whereas most estimates not considering the spatial distribution of the puriglacial slope deposits would be around 355 kg not capable of explaining measured high spatial variability.
机译:由于缺乏对“温室气体”通量的了解,科学的全球变化辩论受到了阻碍。因此,推断土壤衍生的微量气体通量的全球变暖潜能是最大的不确定性来源。在单一的生态系统中,气体通量仍显示出高度可变,因此难以预测。我们的主要论点是,即使在如此详细的范围内,即从地表看,在相当均匀的生态条件下,地貌学也有助于解释大部分的变异性。本论文在Wildmooswald(黑森林/德国西南部)的一个地点进行了测试,该地点最近发现了土壤的单个通量,但不是形成这种多样且主要为水力形态的小圈的原因。当时的想法是,与目前相当均匀的浮雕相比,包括积水层在内的冰缘斜坡沉积物形成了更为复杂的浮雕。从而解释了草皮水气平衡的差异。浸水层由规则的螺旋钻网(25 X 20 m)绘制。全球升温潜势(CH4,N2O)是根据特定土壤的气体特定升温潜势和面积比计算得出的。上部和下部的依存度不一致,因此,冰川周缘斜坡沉积物的释放解释了N2O和CH4排放的空间变异性。研究场平均排放了1059千克二氧化碳当量ha a(-1),而大多数不考虑沿岸坡沉积物空间分布的估计约为355千克,无法解释测得的高空间变异性。

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