Nitrogen accumulation and partitioning in a High Arctic tundra ecosystem from extreme atmospheric N deposition events

被引:29
作者
Choudhary, Sonal [1 ,2 ]
Blaud, Aimeric [1 ]
Osborn, A. Mark [1 ,3 ]
Press, Malcolm C. [4 ,5 ]
Phoenix, Gareth K. [1 ]
机构
[1] Univ Sheffield, Dept Anim & Plant Sci, Western Bank, Sheffield S10 2TN, S Yorkshire, England
[2] Univ Sheffield, Sch Management, Conduit Rd, Sheffield S10 1FL, S Yorkshire, England
[3] RMIT Univ, Sch Appl Sci, POB 71, Bundoora, Vic 3083, Australia
[4] Univ Birmingham, Sch Biosci, Birmingham B15 2TT, W Midlands, England
[5] Manchester Metropolitan Univ, Manchester M15 6BH, Lancs, England
关键词
Extreme nitrogen deposition; Arctic tundra N pools; N immobilisation; N-15; tracer; Plant-soil interactions; Ecosystem N dynamics; MICROBIAL BIOMASS-C; PHOSPHORUS AVAILABILITY; REACTIVE NITROGEN; POLAR SEMIDESERT; NPK FERTILIZER; SOIL MICROBES; FREEZE-THAW; PLANT; RESPONSES; SVALBARD;
D O I
10.1016/j.scitotenv.2016.02.155
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Arctic ecosystems are threatened by pollution from recently detected extreme atmospheric nitrogen (N) deposition events in which up to 90% of the annual N deposition can occur in just a few days. We undertook the first assessment of the fate of N from extreme deposition in High Arctic tundra and are presenting the results from the whole ecosystem N-15 labelling experiment. In 2010, we simulated N depositions at rates of 0, 0.04, 0.4 and 1.2 g N m(-2) yr(-1), applied as (NH4NO3)-N-15-N-15 in Svalbard (79 degrees N), during the summer. Separate applications of (NO3-)-N-15 and (NH4+)-N-15 were also made to determine the importance of N form in their retention. More than 95% of the total N-15 applied was recovered after one growing season (similar to 90% after two), demonstrating a considerable capacity of Arctic tundra to retain N from these deposition events. Important sinks for the deposited N, regardless of its application rate or form, were non-vascular plants N vascular plants N organic soil N litter N mineral soil, suggesting that non-vascular plants could be the primary component of this ecosystem to undergo measurable changes due to N enrichment from extreme deposition events. Substantial retention of N by soil microbial biomass (70% and 39% of N-15 in organic and mineral horizon, respectively) during the initial partitioning demonstrated their capacity to act as effective buffers for N leaching. Between the two N forms, vascular plants (Salix polaris) in particular showed difference in their N recovery, incorporating four times greater (NO3-)-N-15 than (NH4+)-N-15, suggesting deposition rich in nitrate will impact them more. Overall, these findings show that despite the deposition rates being extreme in statistical terms, biologically they do not exceed the capacity of tundra to sequester pollutant N during the growing season. Therefore, current and future extreme events may represent a major source of eutrophication. Crown Copyright (C) 2016 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:303 / 310
页数:8
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