首页> 外文期刊>Global change biology >Soil respiration is stimulated by elevated CO2 and reduced by summer drought: three years of measurements in a multifactor ecosystem manipulation experiment in a temperate heathland (CLIMAITE).
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Soil respiration is stimulated by elevated CO2 and reduced by summer drought: three years of measurements in a multifactor ecosystem manipulation experiment in a temperate heathland (CLIMAITE).

机译:升高的CO 2 刺激了土壤呼吸,夏季干旱降低了土壤呼吸:在温带荒地(CLIMAITE)的多因素生态系统操纵实验中进行了三年的测量。

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This study investigated the impact of predicted future climatic and atmospheric conditions on soil respiration (RS) in a Danish Calluna-Deschampsia-heathland. A fully factorial in situ experiment with treatments of elevated atmospheric CO2 (+130 ppm), raised soil temperature (+0.4 degrees C) and extended summer drought (5-8% precipitation exclusion) was established in 2005. The average RS, observed in the control over 3 years of measurements (1.7 micro mol CO2 m-2 sec-1), increased 38% under elevated CO2, irrespective of combination with the drought or temperature treatments. In contrast, extended summer drought decreased RS by 14%, while elevated soil temperature did not affect RS overall. A significant interaction between elevated temperature and drought resulted in further reduction of RS when these treatments were combined. A detailed analysis of short-term RS dynamics associated with drought periods showed that RS was reduced by ~50% and was strongly correlated with soil moisture during these events. Recovery of RS to pre-drought levels occurred within 2 weeks of rewetting; however, unexpected drought effects were observed several months after summer drought treatment in 2 of the 3 years, possibly due to reduced plant growth or changes in soil water holding capacity. An empirical model that predicts RS from soil temperature, soil moisture and plant biomass was developed and accounted for 55% of the observed variability in RS. The model predicted annual sums of RS in 2006 and 2007, in the control, were 672 and 719 g C m-2 y-1, respectively. For the full treatment combination, i.e. the future climate scenario, the model predicted that soil respiratory C losses would increase by ~21% (140-150 g C m-2 y-1). Therefore, in the future climate, stimulation of C storage in plant biomass and litter must be in excess of 21% for this ecosystem to not suffer a reduction in net ecosystem exchange.
机译:这项研究调查了丹麦 Calluna-Deschampsia R S 上未来气候和大气条件对土壤呼吸的影响/ i>欧石南丛生。完全因子分解原位实验,处理大气中CO 2 升高(+130 ppm),土壤温度升高(+0.4°C)和夏季干旱延长(5-8)于2005年建立了%降水排除率。在3年的测量中,对照中观测到的平均 R S (1.7微摩尔CO < sub> 2 m -2 sec -1 ),在CO 2 升高的情况下增加38%,而与干旱无关或温度处理。相反,长期的夏季干旱使 R S 降低了14%,而土壤温度升高对 R <总体上是i> S 。结合使用这些处理,高温和干旱之间的显着相互作用导致 R S 进一步降低。对干旱时期短期 R S 动力学的详细分析表明, R S 减少了约50%,并且与土壤水分密切相关。 R S 恢复到干旱之前的2周内;但是,在3年中的2年中,在夏季干旱处理后的几个月中观察到了意想不到的干旱影响,这可能是由于植物生长减少或土壤持水量的变化。建立了一个根据土壤温度,土壤水分和植物生物量预测 R S 的经验模型,该模型占观测到的<5>变异的55%。 i> R S 。该模型在对照组中分别预测2006年和2007年 R S 的年总量分别为672和719 g C m -2 y -1 。对于完整的处理组合,即未来的气候情景,该模型预测土壤呼吸碳损失将增加〜21%(140-150 g C m -2 y -1 )。因此,在未来的气候中,植物生态系统中的碳储量的刺激必须超过21%,才能使该生态系统不遭受生态系统净交换的减少。

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