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作为加拿大艾伯塔省油砂开发排放物的指示剂,沼地植物/地衣组织中的氮和硫浓度。

Bog plant/lichen tissue nitrogen and sulfur concentrations as indicators of emissions from oil sands development in Alberta, Canada.

机构信息

Department of Biology, Villanova University, Villanova, PA, 19085, USA.

Center for Biodiversity and Ecosystem Stewardship, Villanova University, Villanova, PA, 19085, USA.

出版信息

Environ Monit Assess. 2021 Mar 23;193(4):208. doi: 10.1007/s10661-021-08929-y.

Abstract

Increasing gaseous emissions of nitrogen (N) and sulfur (S) associated with oil sands development in northern Alberta (Canada) has led to changing regional wet and dry N and S deposition regimes. We assessed the potential for using bog plant/lichen tissue chemistry (N and S concentrations, C:N and C:S ratios, in 10 plant/lichen species) to monitor changing atmospheric N and S deposition through sampling at five bog sites, 3-6 times per growing season from 2009 to 2016. During this 8-year period, oil sands N emissions steadily increased, while S emissions steadily decreased. We examined the following: (1) whether each species showed changes in tissue chemistry with increasing distance from the Syncrude and Suncor upgrader stacks (the two largest point sources of N and S emissions); (2) whether tissue chemistry changed over the 8 year period in ways that were consistent with increasing N and decreasing S emissions from oil sands facilities; and (3) whether tissue chemistry was correlated with growing season wet deposition of NH-N, NO-N, or SO-S. Based on these criteria, the best biomonitors of a changing N deposition regime were Evernia mesomorpha, Sphagnum fuscum, and Vaccinium oxycoccos. The best biomonitors of a changing S deposition regime were Evernia mesomorpha, Cladonia mitis, Sphagnum fuscum, Sphagnum capillifolium, Vaccinium oxycoccos, and Picea mariana. Changing N and S deposition regimes in the oil sands region appear to be influencing N and S cycling in what once were pristine ombrotrophic bogs, to the extent that these bogs may effectively monitor future spatial and temporal patterns of deposition.

摘要

随着加拿大阿尔伯塔省北部油砂开发导致氮 (N) 和硫 (S) 气体排放量的增加,该地区的干湿 N 和 S 沉积模式发生了变化。我们评估了利用沼泽植物/地衣组织化学(10 种植物/地衣物种中的 N 和 S 浓度、C:N 和 C:S 比)来监测大气 N 和 S 沉积变化的潜力,通过在 2009 年至 2016 年期间每生长季节在五个沼泽地站点进行 3-6 次采样。在这 8 年期间,油砂 N 排放量稳步增加,而 S 排放量稳步下降。我们研究了以下几个方面:(1)每种物种的组织化学是否随着与 Syncrude 和 Suncor 升级塔(两个最大的 N 和 S 排放点源)的距离的增加而发生变化;(2)组织化学在 8 年内是否发生了变化,与油砂设施中 N 排放增加和 S 排放减少的情况一致;(3)组织化学是否与生长季节湿沉积的 NH-N、NO-N 或 SO-S 有关。根据这些标准,变化的 N 沉积模式的最佳生物监测器是 Evernia mesomorpha、 Sphagnum fuscum 和 Vaccinium oxycoccos。变化的 S 沉积模式的最佳生物监测器是 Evernia mesomorpha、 Cladonia mitis、 Sphagnum fuscum、 Sphagnum capillifolium、 Vaccinium oxycoccos 和 Picea mariana。油砂地区的 N 和 S 沉积模式的变化似乎正在影响曾经是原始的寡营养沼泽地的 N 和 S 循环,以至于这些沼泽地可能有效地监测未来沉积的空间和时间模式。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/521a/7987692/8f4c72acba15/10661_2021_8929_Fig1_HTML.jpg

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