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慢性大气反应性氮沉积抑制泥炭地中的生物固氮。

Chronic Atmospheric Reactive Nitrogen Deposition Suppresses Biological Nitrogen Fixation in Peatlands.

机构信息

School of Geography, Geology, and the Environment, Keele University, Staffordshire ST5 5BG, United Kingdom.

School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, United Kingdom.

出版信息

Environ Sci Technol. 2021 Jan 19;55(2):1310-1318. doi: 10.1021/acs.est.0c04882. Epub 2021 Jan 4.

Abstract

Biological nitrogen fixation (BNF) represents the natural pathway by which mosses meet their demands for bioavailable/reactive nitrogen (Nr) in peatlands. However, following intensification of nitrogen fertilizer and fossil fuel use, atmospheric Nr deposition has increased exposing peatlands to Nr loading often above the ecological threshold. As BNF is energy intensive, therefore, it is unclear whether BNF shuts down when Nr availability is no longer a rarity. We studied the response of BNF under a gradient of Nr deposition extending over decades in three peatlands in the U.K., and at a background deposition peatland in Sweden. Experimental nitrogen fertilization plots in the Swedish site were also evaluated for BNF activity. In situ BNF activity of peatlands receiving Nr deposition of 6, 17, and 27 kg N ha yr was not shut down but rather suppressed by 54, 69, and 74%, respectively, compared to the rates under background Nr deposition of ∼2 kg N ha yr. These findings were corroborated by similar BNF suppression at the fertilization plots in Sweden. Therefore, contribution of BNF in peatlands exposed to chronic Nr deposition needs accounting when modeling peatland's nitrogen pools, given that nitrogen availability exerts a key control on the carbon capture of peatlands, globally.

摘要

生物固氮 (BNF) 代表了苔藓在泥炭地中满足其对生物可用/反应性氮 (Nr) 需求的自然途径。然而,随着氮肥和化石燃料使用的加剧,大气 Nr 沉积增加,使泥炭地受到 Nr 负荷的影响,通常超过了生态阈值。由于 BNF 是能量密集型的,因此,当 Nr 的可用性不再稀缺时,BNF 是否会关闭尚不清楚。我们研究了在英国三个泥炭地和瑞典一个背景 Nr 沉积泥炭地中,长达数十年的 Nr 沉积梯度下 BNF 的响应,并且还评估了瑞典地点的实验氮施肥地块的 BNF 活性。与背景 Nr 沉积(约 2 kg N ha yr)下的速率相比,接收 6、17 和 27 kg N ha yr Nr 沉积的泥炭地的原位 BNF 活性分别被抑制了 54%、69%和 74%,但并未关闭。这些发现得到了瑞典施肥地块中类似的 BNF 抑制的证实。因此,在对全球范围内泥炭地氮库进行建模时,需要考虑到在长期 Nr 沉积下暴露的泥炭地中 BNF 的贡献,因为氮素的可用性对泥炭地的碳捕获具有关键控制作用。

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