<p>Elevated atmospheric ammonia (NH<sub>3</sub>) concentrations have been reported in the Athabasca Oil Sands Region of Alberta, although the source of these emissions is uncertain. We compiled monthly atmospheric NH<sub>3</sub> data obtained by passive samplers at 45 sites over a 4-year period and found that NH<sub>3</sub> concentrations were greatly elevated above background levels in the summer and were positively correlated with air temperature at sites close (&lt; 15&#xa0;km, n = 16) as well as at sites distant (&gt; 15&#xa0;km, n = 29) from the center of industrial activities. Natural surface waters in the region have not been previously considered as potential NH<sub>3</sub> sources even though the region is dominated by wetlands and small lakes. Measurements of 66 of these lakes showed that 30% have a pH &gt; 8.0 with 3% having a pH &gt; 9.0 that are expected to contain appreciable amounts of NH<sub>3</sub> that can be released to the atmosphere under summertime conditions. Further, most lakes are less than 3&#xa0;m deep and total Kjeldahl N could be as high as 3.5&#xa0;mg&#xa0;L<sup>−1</sup> in shallow lakes and the temperature of the lakes can exceed 20&#xa0;°C in summer, promoting organic matter mineralization and the production of NH<sub>4</sub><sup>+</sup>. We suggest that these conditions can promote the release of NH<sub>3</sub> from natural waterbodies as well as tailings ponds in the summertime and explain the spatial patterns in atmospheric NH<sub>3</sub> that are observed regionally. These emissions need to be better characterized in further studies.</p>

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Surface Waters as a Potential Underestimated Source of Atmospheric Ammonia in the Athabasca Oil Sands Region of Alberta

  • Shaun A. Watmough,
  • Chetwynd Osborne

摘要

Elevated atmospheric ammonia (NH3) concentrations have been reported in the Athabasca Oil Sands Region of Alberta, although the source of these emissions is uncertain. We compiled monthly atmospheric NH3 data obtained by passive samplers at 45 sites over a 4-year period and found that NH3 concentrations were greatly elevated above background levels in the summer and were positively correlated with air temperature at sites close (< 15 km, n = 16) as well as at sites distant (> 15 km, n = 29) from the center of industrial activities. Natural surface waters in the region have not been previously considered as potential NH3 sources even though the region is dominated by wetlands and small lakes. Measurements of 66 of these lakes showed that 30% have a pH > 8.0 with 3% having a pH > 9.0 that are expected to contain appreciable amounts of NH3 that can be released to the atmosphere under summertime conditions. Further, most lakes are less than 3 m deep and total Kjeldahl N could be as high as 3.5 mg L−1 in shallow lakes and the temperature of the lakes can exceed 20 °C in summer, promoting organic matter mineralization and the production of NH4+. We suggest that these conditions can promote the release of NH3 from natural waterbodies as well as tailings ponds in the summertime and explain the spatial patterns in atmospheric NH3 that are observed regionally. These emissions need to be better characterized in further studies.