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Yavapai-Apache
Tribe |
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Chemical components
responsible for haze |
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This analysis assumes that data from the Ike's Backbone
is the most representative IMPROVE site for this area. As shown in Figure 2, the overall average total
light extinction coefficient
(Bext) is 27.6 Mm-1 (Visual Range ~
141 Km; Deciview
~ 10.2).
The average PM2.5 mass concentration is
4.3 mg/m3. The average contributions of the major aerosol
components to Ike's Backbone haze are particulate
sulfate
19.7%,
nitrate 7.6%,
organic
matter (OMC) 14.1%, elemental carbon (light
absorbing carbon, LAC) 5.3%, fine soil
4.7% and
coarse mass (CM) 12.3%.
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Figure 2 Average
contributions of major aerosol chemical components to light extinction
(Based on data available in 1997-2002) |
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As shown in Figure 3, CM is the largest aerosol
contributor to haze in the 20% worst days from April to June, with a
contribution of ~ 25%. Sulfate is the largest aerosol contributor from July
to December, with a contribution of ~ 20 - 25% in the worst days. Nitrate is
the largest aerosol contributor in January and February, with a contribution
of ~ 27% in the worst days. OMC contributes about 15 - 20% to haze in the
worst days from April to November. |
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Figure 3 Average
contributions of major aerosol chemical components to light extinction
during 20% worst days in each month (Based on data available in 1997-2002) |
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For a detailed examination of
the aerosol characteristics at Yavapai-Apache consult the
aerosol description web page. |
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Last updated 8 June 2005
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