Abstract

Abstract. The highest mercury (Hg) wet deposition in the United States of America (USA) occurs along the Gulf of Mexico, and in the southern and central Mississippi River Valley. Gaseous oxidized Hg (GOM) is thought to be a major contributor due to high water solubility and reactivity. Therefore, it is critical to understand concentrations, potential for wet and dry deposition, and GOM compounds present in the air. Concentrations and dry-deposition fluxes of GOM were measured and calculated for Naval Air Station Pensacola Outlying Landing Field (OLF) in Florida using data collected by a Tekran® 2537/1130/1135, the University of Nevada Reno Reactive Mercury Active System (UNRRMAS) with cation exchange and nylon membranes, and the Aerohead samplers that use cation-exchange membranes to determine dry deposition. Relationships with Tekran®-derived data must be interpreted with caution, since the GOM concentrations measured are biased low depending on the chemical compounds in air and interferences with water vapor and ozone.Criteria air pollutants were concurrently measured. This allowed for comparison and better understanding of GOM.In addition to other methods previously applied at OLF, use of the UNRRMAS provided a platform for determination of the chemical compounds of GOM in the air. Results from nylon membranes with thermal desorption analyses indicated seven GOM compounds in this area, including HgBr2, HgCl2, HgO, Hg–nitrogen and sulfur compounds, and two unknown compounds. This indicates that the site is influenced by different gaseous phase reactions and sources. Using back-trajectory analysis during a high-GOM event related to high CO, but average SO2, indicated air parcels moved from the free troposphere and across Arkansas, Mississippi, and Alabama at low elevation (< 300 m). This event was initially characterized by HgBr2, followed by a mixture of GOM compounds. Overall, GOM chemistry indicates oxidation reactions with local mobile source pollutants and long-range transport.In order to develop methods to measure GOM concentrations and chemistry, and model dry-deposition processes, the actual GOM compounds need to be known, as well as their corresponding physicochemical properties, such as Henry's Law constants.

Highlights

  • Mercury (Hg) has been classified as a persistent, bioaccumulative toxin (PBT) (UNEP, 2013), and deposition from the atmosphere is considered the dominant pathway by which highest mercury (Hg) enters remote ecosystems (Lindberg et al, 2007)

  • A contributing factor to wet deposition in the Gulf Coast area may be related to high atmospheric convection during thunderstorms and scavenging of gaseous oxidized Hg (GOM) from the free troposphere (Nair et al, 2013), as well as down-mixing of air with high GOM from the free troposphere (Gustin et al, 2012)

  • Similar to previous work at this location (Gustin et al, 2012), O3 was highest in the spring

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Summary

Introduction

Mercury (Hg) has been classified as a persistent, bioaccumulative toxin (PBT) (UNEP, 2013), and deposition from the atmosphere is considered the dominant pathway by which Hg enters remote ecosystems (Lindberg et al, 2007). In some areas, scavenging by precipitation controls atmospheric Hg removal processes, such as in the southeastern United States of America (USA), where precipitation amounts are high (Prestbo and Gay, 2009). Wet deposition concentrations are not necessarily correlated with precipitation amounts > 81 mm, and deposition has not decreased with emission reductions as coal combustion facilities in the region have implemented control technologies A contributing factor to wet deposition in the Gulf Coast area may be related to high atmospheric convection during thunderstorms and scavenging of gaseous oxidized Hg (GOM) from the free troposphere (Nair et al, 2013), as well as down-mixing of air with high GOM from the free troposphere (Gustin et al, 2012)

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