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Technical Papers

Urban impacts on regional carbonaceous aerosols: Case study in central Texas

&
Pages 917-926 | Received 03 Mar 2014, Accepted 04 Mar 2014, Published online: 16 Jul 2014

Figures & data

Figure 1. Forty-eight-hour back-trajectory plots showing the path of air arriving at Riesel, TX. Spring is shown in red, summer in green, fall in purple, and winter in blue.

Figure 1. Forty-eight-hour back-trajectory plots showing the path of air arriving at Riesel, TX. Spring is shown in red, summer in green, fall in purple, and winter in blue.

Table 1. Comparison of fine particulate matter (PM2.5), organic carbon (OC), elemental carbon (EC), and EC/OC ratios for four sampling sites across Texas for 2011 and 2012

Table 2. Seasonal organic carbon (OC), elemental carbon (EC), organic mass (OM), EC/OC ratio, water-soluble organic carbon (WSOC), and WSOC/OC ratio concentrations for Riesel, TX, for the 15-month sampling campaign from May 2011 to August 2012

Figure 2. Contributions of water-insoluble organic carbon (WIOC), water-soluble organic carbon (WSOC), and elemental carbon by season at Riesel, TX. Average MAC and WSOC MAE365*10 values are also presented. The WSOC MAE365 is not available for spring.

Figure 2. Contributions of water-insoluble organic carbon (WIOC), water-soluble organic carbon (WSOC), and elemental carbon by season at Riesel, TX. Average MAC and WSOC MAE365*10 values are also presented. The WSOC MAE365 is not available for spring.

Table 3. Seasonal averages of elemental carbon light attenuation (EC ATN), elemental carbon mass absorption efficiency (EC MAC), water-soluble organic carbon ATN (WSOC ATN), absorption coefficients of WSOC extracts(WSOC babs), and mass absorption efficiency at 365 nm (WSOC MAE365) of WSOC extracts

Figure 3. Light attenuation vs. filter elemental carbon (EC) loading by season; b[0] is equal to the y-intercept and b[1] is equal to the slope of the regression.

Figure 3. Light attenuation vs. filter elemental carbon (EC) loading by season; b[0] is equal to the y-intercept and b[1] is equal to the slope of the regression.

Figure 4. Scatter plots showing the correlation of WSOC babs (365 nm) and water-soluble organic carbon (WSOC) for summer and winter at Riesel, TX; b[0] is equal to the y-intercept and b[1] is equal to the slope of the regression.

Figure 4. Scatter plots showing the correlation of WSOC babs (365 nm) and water-soluble organic carbon (WSOC) for summer and winter at Riesel, TX; b[0] is equal to the y-intercept and b[1] is equal to the slope of the regression.

Figure 5. Example of water-soluble absorption spectra for one summer (08/13/2012) and one winter (02/15/2012) sample from Riesel, TX. The Angstrom absorption exponent of the summer sample was 5.8, and 4.8 for the winter sample.

Figure 5. Example of water-soluble absorption spectra for one summer (08/13/2012) and one winter (02/15/2012) sample from Riesel, TX. The Angstrom absorption exponent of the summer sample was 5.8, and 4.8 for the winter sample.
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