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首页> 外文期刊>Global change biology >Impacts of an anomalously warm year on soil nitrogen availability in experimentally manipulated intact tallgrass prairie ecosystems
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Impacts of an anomalously warm year on soil nitrogen availability in experimentally manipulated intact tallgrass prairie ecosystems

机译:异常暖年对实验操纵的完整草丛草原生态系统中土壤氮素利用率的影响

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Global climate change can potentially increase the frequency of climate anomalies. Anomalously warm years may cause an increase in soil nitrogen (N) availability by stimulating N mineralization. To date, most studies addressing the effects of ecosystem warming have been conducted in relatively cold ecosystems and few studies have addressed impacts of interannual as opposed to continuous, multiyear warming. In this study, 12 intact soil monoliths were excavated from a tallgrass prairie site near Purcell, Oklahoma, USA and divided among four large flux chambers (EcoCELLs). During the first year, all four EcoCELLs were subjected to Oklahoma air temperatures and precipitation. During the second year, air temperature in two EcoCELLs was increased by 4 pC throughout the year resulting in an increase in soil temperature of 2.3 pC at 7.5 cm depth. During the third and fourth years, temperatures in the warmed EcoCELL returned back to 'normal' conditions. During the warming year, vegetation N content was not significantly affected by the warming treatment suggesting no change in N availability. Other N availability indicators (soil solution chemistry, leaching, and N adsorption by ion exchange resins) did not show any effect of warming. Soil solution, leaching, and ion exchange resins showed a large pulse of NH at the start of the study most likely due to disturbance caused by monolith excavation and transport but these effects were short-lived and had disappeared before the treatment started. The lack of a clear warming effect may be explained by a reduction in soil moisture in the warming treatments compared with the controls offsetting a potential stimulation of N mineralization in response to increased temperatures. As a result, effects of an anomalously warm year on N availability in warmer ecosystems may be small compared with colder ecosystems but are likely to depend on soil moisture status.
机译:全球气候变化可能会增加气候异常的发生频率。异常温暖的年份可能会通过刺激氮矿化而导致土壤氮素的利用率增加。迄今为止,有关生态系统变暖影响的大多数研究都是在相对寒冷的生态系统中进行的,很少有研究涉及年际气候变化而不是持续多年的变暖。在这项研究中,从美国俄克拉荷马州珀塞尔附近的高草草原现场挖出了12个完整的土壤整料,并分成四个大流量室(EcoCELL)。在第一年中,所有四个EcoCELL都受到俄克拉荷马州的气温和降水的影响。在第二年中,两个EcoCELL的空气温度全年升高了4 pC,导致在7.5 cm深度处的土壤温度升高了2.3 pC。在第三和第四年,变暖的EcoCELL中的温度恢复到“正常”状态。在变暖年期间,植被的氮含量不受变暖处理的显着影响,表明氮的有效性没有变化。其他氮素有效性指标(土壤溶液化学性质,淋溶和离子交换树脂对氮的吸附)均未显示出变暖的影响。在研究开始时,土壤溶液,浸出液和离子交换树脂显示出较大的NH脉冲,这很可能是由于整体挖掘和运输引起的干扰,但是这些作用是短暂的,并且在处理开始之前就消失了。缺乏明显的增温作用可以解释为,与对照相比,增温处理中土壤水分的减少抵消了响应于升高的温度而潜在刺激的N矿化。结果,与较寒冷的生态系统相比,异常温暖的一年对较温暖的生态系统中氮的利用率的影响可能较小,但可能取决于土壤水分状况。

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