首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Potassium and phosphorus additions modify the response of Sphagnum capillifolium growing on a Scottish ombrotrophic bog to enhanced nitrogen deposition
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Potassium and phosphorus additions modify the response of Sphagnum capillifolium growing on a Scottish ombrotrophic bog to enhanced nitrogen deposition

机译:钾和磷的添加改变了苏格兰营养养生沼泽上生长的泥炭藓对增强氮沉积的响应

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This study reports the impacts of wet reduced versus oxidised N on in situ responses of Sphagnum capillifolium: architecture, chemistry and F-v/F-m. Nitrogen inputs were enhanced under realistic treatment scenarios in a unique experiment on an ombrotrophic bog ecosystem in the Scottish Borders, UK, receiving, historically and currently, low pollutant deposition. Ammonium (NH4Cl) and nitrate (NaNO3) treatments were applied from 2002 (June) at 16 kg and 64 kg N ha(-1) a(-1) with or without K and P (K2HPO4), provided in a 1: 14 ratio of P:N. These wet treatments were applied to three replicates in precipitation collected at the site, as 'real time' applications to large, 13 m(2) plots. A high application frequency > 100 events was achieved and the maximum spray concentration was 4 mM. Over the study period June 2003-May 2004 rainfall was low over several months enabling the effects of water stress to be looked at. Branching and the length of photosynthetically active material were reduced by the high N input and the effect was more pronounced when the water-table was low, but the form of N was not important. Where the N form was important the effects of oxidised N were less favourable than those of reduced N. The findings are discussed in relation to current knowledge along with implications for critical N loads and management options for bogs to counteract the detrimental impact of elevated N deposition. These results provide further evidence that additions of K and P to N-polluted bogs can ameliorate the direct, negative impacts of N deposition on Sphagnum at least in the short-term. (c) 2007 Elsevier Ltd. All rights reserved.
机译:这项研究报告了湿还原态氮和氧化态氮对泥炭藓的原位响应的影响:结构,化学和F-v / F-m。在英国苏格兰边界的一个营养养护沼泽生态系统的独特实验中,在现实的处理方案下增加了氮的输入,从历史上和目前来看,它们的污染物沉积量都很低。从2002年(6月)开始以16公斤和64公斤N ha(-1)a(-1)施用铵盐(NH4Cl)和硝酸盐(NaNO3)(有或没有钾和磷(K2HPO4),按1:14提供) P:N比这些湿法处理应用于现场收集的降水中的三个重复样本,作为“实时”应用于大型13 m(2)样地。达到了> 100次事件的高施药频率,最大喷雾浓度为4 mM。在2003年6月至2004年5月的研究期内,几个月来降雨量很低,因此可以观察到水分胁迫的影响。高氮输入减少了光合活性物质的分支和长度,当水位较低时,效果更明显,但氮的形式并不重要。当氮的形式很重要时,氧化的氮的影响要比还原的氮的不利。讨论该发现时,结合了当前的知识,以及对临界氮负荷的影响和沼泽的管理方案,以抵消氮沉降增加的不利影响。 。这些结果提供了进一步的证据,证明至少在短期内,向受N污染的沼泽中添加K和P可以减轻N沉积对泥炭的直接负面影响。 (c)2007 Elsevier Ltd.保留所有权利。

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