Critical loads and H+ budgets of forest soils affected by air pollution from oil sands mining in Alberta, Canada

被引:11
|
作者
Jung, Kangho [1 ,2 ]
Chang, Scott X. [1 ]
Ok, Yong Sik [3 ]
Arshad, M. A. [1 ]
机构
[1] Univ Alberta, Dept Renewable Resources, Edmonton, AB T6G 2E3, Canada
[2] Natl Acad Agr Sci, Agr Environm Dept, Suwon 441707, South Korea
[3] Kangwon Natl Univ, Dept Environm Biol, Chunchon 200701, South Korea
基金
加拿大自然科学与工程研究理事会;
关键词
Athabasca oil sands; Critical load; H+ budget; Interception deposition; S deposition; Soil acidification; DEPOSITION; NITROGEN; ACIDIFICATION; WATERSHEDS; SULFUR; REGION; MODEL; ECOSYSTEMS; SATURATION; CHEMISTRY;
D O I
10.1016/j.atmosenv.2012.12.010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We investigated the critical load (CL) and exceedance (EX) of sulfur (S) deposition, temporal changes in soil chemistry, and H+ budget of soils in plots dominated by Pinus banksiana (jack pine) or Populus tremuloides (trembling aspen, aspen) in two acid-sensitive watersheds to assess the risk of soil acidification by S emissions from oil sands mining in the Athabasca oil sands region (AOSR), Canada. The CLs and EXs were determined by two methods: one was based on bulk deposition and the other based on total deposition (as a sum of bulk deposition and interception deposition). The CLs ranged from 223 to 711 mol(c) ha(-1) yr(-1) based on bulk deposition. Those values were similar to that obtained based on total deposition. However, EXs based on bulk deposition were significantly lower (p < 0.001) than those based on total deposition due to the relative increase of SO42- concentrations in interception deposition, indicating that EXs based on bulk deposition only could underestimate the risk of soil acidification in the AOSR. The S deposition did not exceed CLs in the long-term for both methods. The pH in the forest floor increased and available SO42- (as the sum of soluble and adsorbed SO42-) in the forest floor and surface mineral soils increased in both jack pine and aspen stands between 2005 and 2010. The H+ budget ranged from -289 to -130 mole ha(-1) yr(-1) in jack pine stands and from -510 to -371 mol(c) ha(-1) yr(-1) in aspen stands. Our results suggest that 1) soils in the studied forest stands have recovered from acidification based on the increasing soil pH over time and the negative H+ budget, and 2) the risk of soil acidification should be assessed by CL and EX calculated based on total deposition. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:56 / 64
页数:9
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