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In the remainder of zone 3, this estimate was one-third of the maximum plume concentration (in each case, the maximum plume concentration is the maximum of the 8-hr average).
For zone 1, zone 2 and the first 300 feet within zone 3 (nearest the zone 2 boundary), the airborne concentrations from resuspended dust/debris on 11 through 13 September were estimated to be approximately equal to two-thirds of the maximum plume concentration.
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In addition, maximum plume movement and tidal average concentrations are computed.
More than 99%% of the total mass had to be removed in order to lower the plume concentration below the maximum concentration limit (MCL) of 5.0 μg L−1.
The maximum plume height of the cataclysmic eruption was 17000 m a.s.l.l
We use the PlumeRise model of Woodhouse et al. (2013) to estimate the maximum plume height.
Indeed, taking the maximum plume height, the temperature is predicted to fall below −20°C, although the plume height is then significantly higher than the altitude of the highest VHF source (Fig. 9a).
The weather radar gives a maximum plume height of 8.1 km and the atmospheric temperature falls below −20°C, so substantial ice formation is expected.
The realism of the plume model simulations was tested by comparing model calculations of plume concentrations with data of SF6 tracer concentrations and ozone concentrations.
All of these are based on a spatial integration of the plume concentrations above a predefined concentration threshold.
The Hanford Site and the SRS have major plumes containing I at concentrations above the drinking water standard; the former are an order of magnitude larger in size, whereas the latter have orders of magnitude greater I plume concentrations.
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