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Design and Performance of an Atmospheric Reference Standard of Hg 0 and HgCl 2 to Evaluate State-of-the-Art Hg Speciation Measurement Methods. Eric M. Prestbo Frontier Geosciences: Seattle, Washington USA EricP@Frontier.wa.com Robert K. Stevens
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Design and Performance of an Atmospheric Reference Standard of Hg0 and HgCl2 to Evaluate State-of-the-Art Hg Speciation Measurement Methods Eric M. Prestbo Frontier Geosciences: Seattle, Washington USA EricP@Frontier.wa.com Robert K. Stevens Florida DEP at USEPA: Triangle Park, North Carolina USA, Stevens.Robert-K@epamail.epa.gov Steve Lindberg Oak Ridge National Laboratory: Oak Ridge, Tennessee USA sll@ornl.gov F. A. Schaedlich and D. R. Schneeberger Tekran Inc.: Toronto, Ontario Canada fhs@tekran.com Gerald Keeler University of Michigan: Ann Arbor, Michigan USA, jkeeler@sph.umich.edu
Method Development ChallengePrestbo and Bloom, 1996 International Hg Conference, Hamburg • Typical RGM = 20 pg/m3 = 2.2 ppq (quadrillion) • Must minimize possibilities for contamination by using clean equipment and handling protocols • Rule out Hg0 Hg(II) transformations during sampling • Rule out Hg(II) loss during sampling, storage or analysis • Is relative humidity important?
RGM Instrument Design Requirements • Method must be 1-2 orders of magnitude more sensitive than total Hg method • Must reject much larger Hg0 component • Exclude particulate bound Hg, however particulate filters can adsorb RGM • Instrument must pass RGM to the collector quantitatively • Automated to exclude handling contamination and provide high time resolution.
Crux of the Problem • To rigorously evaluate any RGM method, we need to have a laboratory system capable of generating quantified, constant, low, pg/m3 concentrations of HgCl2 and Hg0 in various atmospheric matrices. • Critically important to prove that there is no conversion of Hg0 to RGM.
Results Summary • Capillary diffusion of HgCl2 from dodecane not initially effective • Heated URG-Teflon coated manifold greatly minimizes HgCl2 sticking and memory effect. • Ice-bath HgCl2 permeation source - poor temperature control at interface with heated manifold • No Hg0 observed in HgCl2 permeation source
Results Summary • Addition of %RH to manifold helped to reduce sticking of HgCl2, but also converted HgCl2 to Hg0 in system • Zero Hg system blanks with both cylinder N2, ambient air with gold scrubber and addition of %RH from bubblers • Real-time calibration with thermal conversion KCl-coated annular denuder
Results Summary • Responds to HgCl2 quantitatively • Blanks <1 pg/m3, Two-system method precision <10%, Est. DL = 1 pg/m3 • No HgCl2 breakthrough at high levels • Rugged - Operated for 10 days unattended • High sample frequency will allow for observation of anthropogenic source plumes
Results Summary • Addition of 80 ppbv of O3 to ~10 ng/m3 Hg0 produced a conversion to RGM of 0.13% = only a 2.6 pg/m3 bias at the 2 ng/m3 level • Field spiking/calibration method works well in laboratory - yet needs refinement • Future work will focus on application of the calibration/spiking method in the field
Mercury Nomenclature • TGM - Total Gaseous Mercury -Hg0 + Hg(II)? • GEM - Total Gaseous Elemental Mercury- Hg0 • TPM - Total Particulate Mercury - Hgp • RGM - Reactive Gaseous Mercury - HgCl2?
Purpose of Research: Big Picture • To quantify how much of the Hg deposition to sensitive aquatic ecosystems is the result of local, regional and global emissions sources of Hg. • Current understanding of the problem requires that we quantify atmospheric Hg species, Hg0, particulate Hg (PHg) and gas-phase Hg(II) - RGM.
Why Measure RGM • RGM (likely HgCl2) is emitted from coal combustion and waste incineration sources • RGM formed in atmosphere via oxidation by O3, Cl2 and likely heterogeneous rxns. • Atmospheric models predict that RGM dominates wet and dry deposition: Models are highly sensitive to RGM emissions and atmospheric concentrations
Purpose of Research: Detailed Picture • Build a laboratory system capable of generating atmospheric test matrices to calibrate and challenge the Tekran RGM Method • Develop a means to evaluate and calibrate the Tekran RGM method in the field.
Technical Challenges for Building a Laboratory RGM Test System • HgCl2 has a high sticking coefficient • Inert surfaces must be everywhere • Elevated and constant temperature • System blanks at the sub-pg/m3 level with both cylinder air, ambient air and RH addition • Absolute purity of Hg0 and HgCl2 sources • Monitoring HgCl2 levels in real-time
From Mercury over Europe (MOE) Campaign Courtesy of GKSS and IVL
Field Calibration • 10 l of Hg(II)/hexane is injected into cup at heated denuder inlet • Hexane and Hg(II) evaporate into KCl annular denuder as a calibration with zero air OR matrix spike in ambient air
GOM Calibration ResearchRevisited ~2004-2006Dynamic Injection&Denuder Spiking
Schematic of RGM Calibration Method alkane (l) > alkane (g) 9 lpm or 90% of alkane exhausted to air HgCl2 adsorbs to denuder Inject 10 ul of HgCl2 in alkane 1 lpm or 10% of alkane through detector
Phase II – Heated Calibration Cup Standard Inlet Standard Denuder
www.tekran.com lab-air-info@tekran.com Success: transfer efficiency, high wall temp
Denuder SpikingHgCl2 Applied to Denuder Installed in 1130 and Desorbed
Denuder Spiking with HgCl2(Olson – USGS & Kilner – Tekran) • Tests: accuracy of the GOM thermal desorption, line transfer, and quantification • 48.4 pg HgCl2 was added to each denuder, then shipped overnight for analysis the following day. • Each experiment had one blank for each instrument. • Four instruments were used in the experiments. GOM Surrogate Spiked Denuder