4.7 Article

Are bog plant/lichen tissue concentrations of Ca, Mg, K, and P affected by fugitive dust released from oil sands development in the Fort McMurray region of Alberta?

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 849, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.scitotenv.2022.157684

关键词

Base cations; Bog; Dust; Oil sands; Phosphorus; Vegetation

资金

  1. Oil Sands Monitoring Program [18GRAEM07]
  2. Villanova University Falvey Memorial Library Scholarship Open Access Reserve (SOAR) Fund

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Bogs rely on atmospheric deposition for new elements. Increased element deposition from human activities can alter nutrient availability and ecosystem function in bogs. Bogs may function as effective monitors of element deposition. By quantifying plant/lichen tissue concentrations, the potential effects of fugitive dust from oil sands development in Alberta, Canada were assessed. Calcium and magnesium deposition decreased with distance from the oil sands industrial center, while potassium and phosphorus deposition did not. Calcium and magnesium concentrations in tissues decreased with distance. Deposition of calcium and magnesium were positively correlated with tissue concentrations in most species. Tissue concentrations of potassium and phosphorus were not correlated with deposition.
Bogs are ombrotrophic, relying solely on atmospheric deposition for new inputs of elements. Increased element deposition through anthropogenic activities has the potential to alter nutrient availability, and hence ecosystem function, in bogs. Further, because of efficient element retention, bogs may function as effective monitors of element deposition. To assess the potential effects of particulate fugitive dust from oil sands development in Alberta, Canada, we quantified plant/lichen tissue Ca, Mg, K, and P concentrations in 6 bogs ranging from 12 to 77 km from the oil sands industrial center. Deposition of Ca and Mg, but not K or P, quantified using ion exchange resin collectors, to bogs decreased with distance from the oil sands industrial center. Concentrations of Ca and Mg, but not K or P, in tissues of lichens (Cladonia mitis, Evernia mesomorpha) and Sphagnum (S. capillifolium, S. fuscum) decreased with distance from the oil sands industrial center. Tissue Ca concentrations were positively correlated with growing season Ca and Mg deposition in all species except Vaccinium oxycoccos, Rhododendron groenlandicum, and Picea mariana; leaf Mg concentrations were positively correlated with growing season Mg deposition for all species except P. mariana. Tissue concentrations of K and P were not correlated with growing season K and P deposition. For each species, receptor modeling identified two distinct sources, one dominated by Ca and Mg, presumed to represent particulate fugitive dust from oil sands activities, and a second dominated by K and P, which may reflect tight internal cycling and upward translocation of K and P in peat and/or K and P deposition as particulates generated in wildfires. Increasing Ca2+ and Mg2+ deposition may acidify bog porewaters through cation exchange in peat.

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