Tracing industrial sulfur contributions to atmospheric sulfate deposition in the Athabasca oil sands region, Alberta, Canada

被引:40
|
作者
Proemse, Bernadette C. [1 ]
Mayer, Bernhard [1 ]
Fenn, Mark E. [2 ]
机构
[1] Univ Calgary, Dept Geosci, Calgary, AB T2N 1N4, Canada
[2] US Forest Serv, USDA, Pacific SW Res Stn, Riverside, CA 92507 USA
基金
加拿大自然科学与工程研究理事会;
关键词
ACID DEPOSITION; ISOTOPIC COMPOSITION; PHASE OXIDATION; OXYGEN; PRECIPITATION; NITROGEN; RATIOS; FOREST; O-18; ACIDIFICATION;
D O I
10.1016/j.apgeochem.2012.08.006
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Anthropogenic S emissions in the Athabasca oil sands region (AOSR) in Alberta, Canada, affect SO4 deposition in close vicinity of industrial emitters. Between May 2008 and May 2009, SO4-S deposition was monitored using open field bulk collectors at 15 sites and throughfall collectors at 14 sites at distances between 3 and 113 km from one of the major emission stacks in the AOSR. At forested plots >90 km from the operations, SO4 deposition was similar to 1.4 kg SO4-S ha (1) yr (1) for bulk deposition and similar to 3.3 kg SO4-S ha (1) yr (1) for throughfall deposition. Throughfall SO4 deposition rates in the AOSR exceeded bulk deposition rates at all sites by a factor of 2-3, indicating significant inputs of dry deposition especially under forest canopies. Both bulk and throughfall SO4 deposition rates were elevated within 29 km distance of the industrial operations with deposition rates as high as 11.7 kg SO4-S ha (1) yr (1) for bulk deposition and 39.2 kg SO4-S ha (1) yr (1) for throughfall at industrial sites. Sulfur isotope ratio measurements of atmospheric SO4 deposited in the AOSR revealed that at a few selected locations S-34-depleted SO4, likely derived from H2S emissions from tailing ponds contributes to local atmospheric SO4 deposition. In general, however, delta S-34 values of SO4 deposition at distant forested plots (>74 km) with low deposition rates were not isotopically different from delta S-34 values at sites with high deposition rates in the AOSR and are, therefore, not suitable to determine industrial S contributions. However, O isotope ratios of atmospheric SO4 in bulk and throughfall deposition in the AOSR showed a distinct trend of decreasing delta O-18-SO4 values with increasing SO4 deposition rates allowing quantification of industrial contributions to atmospheric SO4 deposition. Two-end-member mixing calculations revealed that open field bulk SO4 deposition especially at industrial sites in close proximity (<29 km) to the operations is significantly (17-59%) affected by industrial S emissions and that throughfall generally contained 49-100% SO4 of industrial origin. Hence, it is suggested that delta O-18 values of SO4 may constitute a suitable tracer for quantifying industrial contributions to atmospheric SO4 deposition in the AOSR. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2425 / 2434
页数:10
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