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首页> 外文期刊>Global change biology >Effects of extreme experimental drought and rewetting on CO2 and CH4 exchange in mesocosms of 14 European peatlands with different nitrogen and sulfur deposition
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Effects of extreme experimental drought and rewetting on CO2 and CH4 exchange in mesocosms of 14 European peatlands with different nitrogen and sulfur deposition

机译:极端实验性干旱和再湿润对14种不同氮和硫沉积量的欧洲泥炭地中地膜CO2和CH4交换的影响

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The quantitative impact of intense drought and rewetting on gas exchange in ombrotrophic bogs is still uncertain. In particular, we lack studies investigating multitudes of sites with different soil properties and nitrogen (N) and sulfur (S) deposition under consistent environmental conditions. We explored the timing and magnitude of change in CO2 (Respiration, Gross Primary Production - GPP, and Net Exchange - NE) and CH4 fluxes during an initial wet, a prolonged dry (similar to 100 days), and a subsequent wet period (similar to 230 days) at 12 degrees C in 14 Sphagnum peat mesocosms collected in hollows from bogs in the UK, Ireland, Poland, and Slovakia. The relationship of N and S deposition with GPP, respiration, and CH4 exchange was investigated. Nitrogen deposition increased CO2 fluxes and GPP more than respiration, at least up to about 15 kg N ha(-1) yr(-1). All mesocosms became CO2 sources during drying and most of them when the entire annual period was considered. Response of GPP to drying was faster than that of respiration and contributed more to the change in NE; the effect was persistent and few sites recovered "predry" GPP by the end of the wet phase. Respiration was higher during the dry phase, but did not keep increasing as WT kept falling and peaked within the initial 33 days of drying; the change was larger when differences in humification with depth were small. CH4 fluxes strongly peaked during early drought and water table decline. After rewetting, methanogenesis recovered faster in dense peats, but CH4 fluxes remained low for several months, especially in peats with higher inorganic reduced sulfur content, where sulfate was generated and methanogenesis remained suppressed. Based on a range of European sites, the results support the idea that N and S deposition and intense drought can substantially affect greenhouse gas exchange on the annual scale.
机译:强烈干旱和再湿润对非营养营养沼泽中气体交换的定量影响仍然不确定。尤其是,我们缺乏研究来研究在一致的环境条件下具有不同土壤特性以及氮(N)和硫(S)沉积的众多地点。我们探讨了在最初的潮湿,长时间的干燥(大约100天)和随后的潮湿时期(相似的时间)期间,CO2(呼吸,初级总产值-GPP和净交换-NE)和CH4通量变化的时间和幅度。到230天)是在12摄氏度下从英国,爱尔兰,波兰和斯洛伐克的沼泽中收集到的14个泥炭泥炭中观。研究了氮和硫沉积与GPP,呼吸作用和CH4交换的关系。氮沉积比呼吸作用更多地增加了CO2通量和GPP,至少高达约15 kg N ha(-1)yr(-1)。在干燥过程中,所有中观宇宙都变成了CO2的来源,其中大部分是在考虑整个全年的过程中变成的。 GPP对干燥的反应比呼吸更快,并且对NE的变化贡献更大。这种影响是持久的,到湿阶段结束时,几乎没有站点恢复“预干燥” GPP。在干燥阶段,呼吸较高,但由于WT在干燥的最初33天内不断下降并达到峰值而没有持续增加。当腐殖化的深度差异较小时,变化较大。在早期干旱和地下水位下降期间,CH4通量强烈达到峰值。重新润湿后,致密泥炭中甲烷生成的恢复速度更快,但CH4流量却保持了几个月的低位,尤其是在无机物含量降低的硫含量较高的泥炭中,生成了硫酸盐且甲烷生成仍被抑制。基于一系列欧洲站点,研究结果支持了氮和硫的沉积以及强烈的干旱会在很大程度上影响温室气体交换的观点。

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