Abstract

Abstract. Source apportionment analysis was conducted with positive matrix factorization (PMF) and principal component analysis (PCA) methods using concentrations of speciated mercury (Hg), i.e., gaseous elemental mercury (GEM), gaseous oxidized mercury (GOM), and particulate-bound mercury (PBM), and other air pollutants collected at Kejimkujik National Park, Nova Scotia, Canada, in 2009 and 2010. The results were largely consistent between the 2 years for both methods. The same four source factors were identified in each year using PMF method. In both years, factor photochemistry and re-emission had the largest contributions to atmospheric Hg, while the contributions of combustion emission and industrial sulfur varied slightly between the 2 years. Four components were extracted with air pollutants only in each year using PCA method. Consistencies between the results of PMF and PCA include (1) most or all PMF factors overlapped with PCA components, (2) both methods suggest strong impact of photochemistry but little association between ambient Hg and sea salt, and (3) shifting of PMF source profiles and source contributions from one year to another was echoed in PCA. Inclusion of meteorological parameters led to identification of an additional component, Hg wet deposition in PCA, while it did not affect the identification of other components. The PMF model performance was comparable in 2009 and 2010. Among the three Hg forms, the agreements between model-reproduced and observed annual mean concentrations were excellent for GEM, very good for PBM, and acceptable for GOM. However, on a daily basis, the agreement was very good for GEM but poor for GOM and PBM. Sensitivity tests suggest that increasing sample size by imputation is not effective in improving model performance, while reducing the fraction of concentrations below method detection limit, by either scaling GOM and PBM to higher concentrations or combining them to reactive mercury, is effective. Most of the data treatment options considered had little impact on the source identification or contribution.

Highlights

  • Atmospheric mercury (Hg) exists in the form of gaseous elemental Hg (GEM) and oxidized Hg, the latter can be in gaseous phase or associated with particulate matter

  • Some of the dry and wet deposited particulate-bound mercury (PBM) and gaseous oxidized mercury (GOM) will be reduced to GEM in soil, water, and vegetation surfaces where Hg will be re-emitted in the form of GEM to the atmosphere (Gaffney and Marley, 2014)

  • Source apportionment analysis was conducted with positive matrix factorization (PMF) and principal component analysis (PCA) using concentrations of speciated Hg and other air pollutants collected at KEJ site in 2009 and 2010

Read more

Summary

Introduction

Atmospheric mercury (Hg) exists in the form of gaseous elemental Hg (GEM) and oxidized Hg, the latter can be in gaseous phase (gaseous oxidized Hg – GOM) or associated with particulate matter (particulate-bound Hg – PBM). Atmospheric Hg can be produced from anthropogenic activities, natural events, and re-emission of previously deposited Hg; the latter two are sometimes grouped together as natural emission sources (Gustin et al, 2008; Pirrone et al, 2010; UNEP, 2013; Gaffney and Marley, 2014; Zhang et al, 2016). X. Xu et al.: Sources and processes affecting atmospheric Hg at Kejimkujik National Park, Canada mining, mining and smelting, and coal combustion are the three major anthropogenic sources (UNEP, 2013; Zhang et al, 2016). Some of the dry and wet deposited PBM and GOM will be reduced to GEM in soil, water, and vegetation surfaces where Hg will be re-emitted in the form of GEM to the atmosphere (Gaffney and Marley, 2014). The contributions of each source and process to a given receptor site are affected by many factors including proximity to sources and weather conditions

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call