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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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Along with predicted climate change, increased risks for summer drought areprojected for Central Europe. However, large knowledge gaps exist in termsof how drought events influence the short-term ecosystem carbon cycle. Here,we present results from 13CO2 pulse labeling experiments at anintensively managed lowland grassland in Switzerland. We investigated theeffect of extreme summer drought on the short-term coupling of freshlyassimilated photosynthates in shoots to roots as well as to soil CO2efflux.Summer drought was simulated using rainout shelters during two field seasons(2010 and 2011). Soil CO2 efflux and its isotopic composition weremeasured with custom-built chambers coupled to a quantum cascade laserspectrometer (QCLAS-ISO, Aerodyne Research Inc., MA, USA). During the 90 minpulse labeling experiments, we added 99.9 atom % 13CO2 to thegrass sward. In addition to the isotopic analysis of soil CO2 efflux,this label was traced over 31 days into bulk shoots, roots and soil.Drought reduced the incorporation of recently fixed carbon into the shoots,but increased the relative allocation of fresh assimilates below groundcompared to the control grasslands. Contrary to our hypothesis, we did notfind a change of allocation speed in response to drought. Although droughtclearly reduced soil CO2 efflux rates, about 75% of total traceruptake in control plots was lost via soil CO2 efflux during 19 daysafter pulse labeling, compared to only about 60% under droughtconditions. Thus, the short-term coupling of above- and below-groundprocesses was reduced in response to summer drought. The occurrence of anatural spring drought in 2011 lead to comparable albeit weaker droughtresponses increasing the confidence in the generalizability of our findings.
机译: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,在干旱事件如何影响短期生态系统碳循环方面,存在巨大的知识空白。在此,我们介绍了在瑞士集约化管理的低地草原上, 13 CO 2 脉冲标记实验的结果。我们研究了极端夏季干旱对嫩芽中新同化光合产物与根以及土壤CO 2 外流短期耦合的影响。 在降雨期间使用雨棚模拟了夏季干旱两个野外季节(2010年和2011年)。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分钟脉冲标记实验中,我们将99.9原子%的 13 CO 2 添加到草丛中。除了对土壤CO 2 外流进行同位素分析外,该标签还可以在31天之内追溯到大块茎,根和土壤中。 干旱减少了最近固定的碳向土壤中的吸收。但与对照草地相比,地下新鲜同化物的相对分配增加了。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,但在脉冲标记后的19天中,对照地块中约75%的总迹线损失是通过土壤CO 2 的外流而损失的,而仅60 %在干旱条件下。因此,响应夏季干旱,减少了地上和地下过程的短期耦合。尽管干旱反应较弱,但2011年春季自然干旱的发生导致可比的结果增加了人们对我们研究结果推广的信心。

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