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FIELD TESTING AND EVALUATION OF DUST DEPOSITION AND ...

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value which was used up to the midpoint between the second and third measurement, and<br />

so on.<br />

6.2.3 Calculation of Horizontal Flux<br />

The power law wind profile is appealing since analytical solutions exist for the<br />

integral of a power law for wind with either an exponential or a Gaussian function for<br />

dust concentration. For the exponential dust concentration case:<br />

F dust =<br />

<br />

C(z) u(z) dz =<br />

∞<br />

( Ae − Bz)<br />

<br />

<br />

z<br />

u ref<br />

<br />

<br />

0<br />

z ref<br />

<br />

<br />

<br />

P<br />

<br />

− P Γ( P +1)<br />

dz = Au ref z ref<br />

<br />

B ( P+1)<br />

Equation 6-4<br />

where Γ is the gamma function. Using a mathematical model that results in a converging<br />

definite integral avoids any uncertainty about the upper limit of integration, z max . The<br />

integral of a power law for wind, times a power law for dust concentration has an analytic<br />

solution, but does not converge. For this study, the horizontal dust flux was also<br />

calculated by trapezoidal rule numerical integration of Equation 6-1 using alternative<br />

interpolation equations to model the time averaged wind speed and concentration as a<br />

function of height. Variable step size (starting at ∆z = 0.1 m) was used to provide higher<br />

resolution near the ground where both concentration and wind speed change rapidly with<br />

height.<br />

6.3 Results<br />

The data were collected during two vehicle activity periods between 01:00 and<br />

02:30 Mountain Daylight Time on September 26, 2001. The clear sky, nighttime, desert<br />

conditions resulted in a stable atmosphere during the sampling period. Wind speed was<br />

generally between 1 and 5 m s -1 , which was sufficient to move the dust cloud, and the<br />

wind direction relative remained within 45° of perpendicular to the container array and<br />

road. General meteorological data are summarized in Table 6-2. Table 6-3 gives the<br />

wind speed and dust concentration mean and standard deviation.<br />

Table 6-2 Meteorological data from station DPG08, approximately 1 km south of test site, for<br />

September 26, 2002 01:00-03:00 MDT.<br />

Average Range<br />

Temperature 294 K 293 - 297 K<br />

Relative Humidity 23% 20-26%<br />

Barometric Pressure<br />

866.54 mbar<br />

24 hr- Precipitation 0<br />

Wind at 10 m 3.0 m s -1 15 m s -1 gust<br />

Wind Direction from True North 98-186°<br />

6-4

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