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首页> 外文期刊>Global change biology >Increased nitrate availability in the soil of a mixed mature temperate forest subjected to elevated CO2 concentration (canopy FACE)
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Increased nitrate availability in the soil of a mixed mature temperate forest subjected to elevated CO2 concentration (canopy FACE)

机译:受CO2浓度升高(冠层FACE)的影响,混合温带森林成熟土壤中硝酸盐的利用率增加

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In a mature temperate forest in Hofstetten, Switzerland, deciduous tree canopies were subjected to a free-air CO2 enrichment (FACE) for a period of 8-years. The effect of this treatment on the availability of nitrogen (N) in the soil was assessed along three transects across the experimental area, one under Fagus sylvatica, one under Quercus robur and Q. petraea and one under Carpinus betulus. Nitrate, ammonium and dissolved organic N (DON) were analysed in soil solution obtained with suction cups. Nitrate and ammonium were also captured in buried ion-exchange resin bags. These parameters were related to the local intensity of the FACE treatment as measured from the 13C depletion of dissolved inorganic carbon in the soil solution. Over the 8-years of experiment, the CO2 enrichment reduced DON concentrations, did not affect ammonium, but induced higher nitrate concentrations, both in soil solution and resin bags. In the nitrate captured in the resin bags, the natural abundance of the isotope 15N increased strongly. This indicates that the CO2 enrichment accelerated net nitrification, probably as an effect of the higher soil moisture resulting from the reduced transpiration of the CO2-enriched trees. It is also possible that N mineralization was enhanced by root exudates (priming effect) or that the uptake of inorganic N by these trees decreased slightly as the result of a reduced N demand for fine-root growth. In this mature deciduous forest, we did not observe any progressive N limitation due to elevated atmospheric CO2 concentrations; on the contrary, we observed an enhanced N availability over the 8-years of our measurements. This may, together with the global warming projected, exacerbate problems related to N saturation and nitrate leaching, although it is uncertain how long the observed trends will last in the future.
机译:在瑞士霍夫斯特滕一个成熟的温带森林中,落叶树冠层进行了8年的自由空气CO2富集(FACE)。沿实验区域的三个样带评估了该处理对土壤中氮(N)有效性的影响,其中一个样带在草地青冈下,一个在白栎和栎下,在一个甜菜下。在用吸盘获得的土壤溶液中分析了硝酸盐,铵盐和溶解的有机氮(DON)。硝酸盐和铵也被捕获在埋入的离子交换树脂袋中。这些参数与FACE处理的局部强度有关,该强度是从土壤溶液中溶解的无机碳的13C损耗测量的。在8年的实验中,CO2富集降低了土壤溶液和树脂袋中的DON浓度,不影响铵盐,但诱导了较高的硝酸盐浓度。在树脂袋中捕获的硝酸盐中,同位素15N的自然丰度大大增加。这表明CO2的富集加速了净硝化作用,这可能是由于富含CO2的树木蒸腾作用减少而导致的土壤湿度更高的结果。根系分泌物可能增强了氮的矿化作用(引发作用),或者由于减少了对细根生长的氮需求,这些树木对无机氮的吸收略有减少。在这个成熟的落叶林中,由于大气中CO2浓度升高,我们没有观察到任何进行性N限制。相反,我们在8年的测量中观察到氮的利用率提高。尽管尚不确定观察到的趋势将持续多久,但这可能与预计的全球变暖加剧了与氮饱和和硝酸盐浸出有关的问题。

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