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The impact of extreme summer drought on the short-term carbon coupling of photosynthesis to soil COsub2/sub efflux in a temperate grassland

机译:夏季极端干旱对温带草原光合作用的短期碳耦合与土壤CO 2 外排的影响

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pstrongAbstract./strong Along with predicted climate change, increased risks for summer drought are projected for Central Europe. However, large knowledge gaps exist in terms of how drought events influence the short-term ecosystem carbon cycle. Here, we present results from sup13/supCOsub2/sub pulse labeling experiments at an intensively managed lowland grassland in Switzerland. We investigated the effect of extreme summer drought on the short-term coupling of freshly assimilated photosynthates in shoots to roots as well as to soil COsub2/sub efflux. brbr Summer drought was simulated using rainout shelters during two field seasons (2010 and 2011). Soil COsub2/sub efflux and its isotopic composition were measured with custom-built chambers coupled to a quantum cascade laser spectrometer (QCLAS-ISO, Aerodyne Research Inc., MA, USA). During the 90 min pulse labeling experiments, we added 99.9 atom % sup13/supCOsub2/sub to the grass sward. In addition to the isotopic analysis of soil COsub2/sub efflux, this label was traced over 31 days into bulk shoots, roots and soil. brbr Drought reduced the incorporation of recently fixed carbon into the shoots, but increased the relative allocation of fresh assimilates below ground compared to the control grasslands. Contrary to our hypothesis, we did not find a change of allocation speed in response to drought. Although drought clearly reduced soil COsub2/sub efflux rates, about 75% of total tracer uptake in control plots was lost via soil COsub2/sub efflux during 19 days after pulse labeling, compared to only about 60% under drought conditions. Thus, the short-term coupling of above- and below-ground processes was reduced in response to summer drought. The occurrence of a natural spring drought in 2011 lead to comparable albeit weaker drought responses increasing the confidence in the generalizability of our findings./p.
机译:> >摘要。随着预计的气候变化,预计中欧夏季干旱的风险会增加。但是,就干旱事件如何影响短期生态系统碳循环而言,存在巨大的知识空白。在这里,我们介绍了在瑞士一个集约化管理的低地草原上, 13 CO 2 脉冲标记实验的结果。我们研究了夏季极端干旱对芽中新鲜吸收的光合产物与根以及土壤CO 2 外流短期耦合的影响。 在两个田间季节(2010年和2011年)使用防雨棚模拟了夏季干旱。使用与量子级联激光光谱仪(QCLAS-ISO,Aerodyne Research Inc.,MA,美国)耦合的定制腔室测量土壤CO 2 的流出量及其同位素组成。在90分钟的脉冲标记实验中,我们向草皮中添加了99.9%的原子 13 CO 2 。除了对土壤CO 2 外排进行同位素分析外,该标记还可以在31天之内追溯到大苗,根和土壤中。 与对照草原相比,干旱减少了新近固定碳在苗中的吸收,但增加了地下新鲜同化物的相对分配。与我们的假设相反,我们没有发现干旱响应分配速度的变化。尽管干旱明显降低了土壤CO 2 的外排率,但与脉冲标记相比,在19天的对照样地中,土壤中CO 2 的外排量损失了示踪剂吸收总量的75%。在干旱条件下只有大约60%。因此,响应夏季干旱,减少了地上和地下过程的短期耦合。 2011年的自然春季干旱的发生导致可比的干旱响应,尽管干旱响应较弱,从而增强了我们对研究结果的普遍性的信心。

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