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长期氮磷富集会改变旱地土壤的植被物种组成,并减少碳储量。

Long-term nitrogen and phosphorus enrichment alters vegetation species composition and reduces carbon storage in upland soil.

机构信息

Institute of Biological, Environmental and Rural Sciences, Penglais Campus, Aberystwyth University, Wales SY23 3DD, United Kingdom.

Centre for Ecology & Hydrology, Bangor, Environment Centre Wales, Bangor LL57 2UP, United Kingdom.

出版信息

Sci Total Environ. 2017 Sep 1;593-594:688-694. doi: 10.1016/j.scitotenv.2017.03.136. Epub 2017 Mar 30.

Abstract

Reactive nitrogen (N) deposition can affect ecosystem processes, particularly in oligotrophic upland habitats. Phosphorus (P) addition has been proposed to reduce the effects of N enrichment on N leaching and acidification, since P limitation can reduce biomass production and consequent sequestration of reactive N. However, biodiversity is often reduced in more productive ecosystems and P limitation may protect against this effect. Responses to P availability in instances of high N deposition are poorly understood. This study investigated the ecosystem response to alleviation of P limitation, using a long-term nutrient addition experiment (1996-2012) three years after ceasing N inputs and 15years after a single P application. Substantial differences were observed in the structure and composition of vegetation species and above-ground vegetation biomass. Vegetation height was greater in the N+P addition treatments (+38% cf. control), with increased cryptogam cover (+47%), whereas N addition increased graminoid species cover (+68%). Vegetation diversity was significantly reduced by the addition of P (-21%), indicating that P limitation is likely to be an important mechanism that limits biodiversity loss in upland habitats exposed to chronic N deposition. Significant differences in soil C and N contents were also observed between treatments. Relative to control, the addition of N increased soil C (+11%) and N (+11%) pool sizes, whereas the addition of N and P reduced soil C (-12%) and N (-13%) pool sizes. This demonstrated the importance of P availability for upland ecosystem processes, and highlights the long-term effects of P addition on vegetation species composition and C storage. Thus, the addition of P cannot be endorsed as a method for reducing impacts of N deposition. Capsule: Phosphorus limitation is a major mechanism governing ecosystem processes in situations of high atmospheric nitrogen deposition.

摘要

活性氮(N)沉积会影响生态系统过程,特别是在贫营养的高地生境中。已有人提议添加磷(P)以减少 N 富集对 N 淋溶和酸化的影响,因为 P 限制可以减少生物量的产生,并因此减少活性 N 的固定。然而,在生产力较高的生态系统中,生物多样性往往会减少,而 P 限制可能会防止这种效应。在高 N 沉积的情况下,对 P 可用性的响应尚不清楚。本研究通过一项长期养分添加实验(1996-2012 年),在停止 N 输入三年后和单次 P 应用后 15 年,调查了生态系统对缓解 P 限制的响应。在植被物种结构和组成以及地上植被生物量方面观察到了显著差异。N+P 添加处理的植被高度更高(+38%,与对照相比),隐花植物覆盖度增加(+47%),而 N 添加增加了禾本科植物的覆盖度(+68%)。P 添加显著降低了植被多样性(-21%),表明 P 限制可能是限制暴露于慢性 N 沉积的高地生境生物多样性丧失的一个重要机制。处理之间的土壤 C 和 N 含量也存在显著差异。与对照相比,N 添加增加了土壤 C(+11%)和 N(+11%)库大小,而 N 和 P 的添加减少了土壤 C(-12%)和 N(-13%)库大小。这表明 P 可用性对高地生态系统过程的重要性,并强调了 P 添加对植被物种组成和 C 储存的长期影响。因此,不能将 P 添加作为减少 N 沉积影响的方法。

注释

  1. 原文中“capsule”一段为对全文的总结,并非翻译内容,可省略不译。

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