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In NFPA 92B, Morton's integral equation was introduced for calculating the maximum plume rise, and beam smoke detectors were recommended for smoke detection design.
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The flux measurements were then incorporated into an ash plume rise model, to calculate the maximum height of the eruptive column, and assess its atmospheric dispersal.
The peak value of velocity provides the input for a numerical model of plume rise.
The estimated eruption velocities serve as the input for numerical models of plume rise.
Comparisons of the predicted results with experimental data show good agreement for the plume rise.
One of the sites consists of Quaternary unconsolidated sand with a high porosity and permeability, allowing fast CO2 plume rise and the possibility of creating chimney-like plumes.
Subsequently, Briggs modified his 1969 plume rise equations in 1971 and in 1972.
G. A. Briggs first published his plume rise observations and comparisons in 1965.
That was followed in 1969 by his classical critical review of the entire plume rise literature, in which he proposed a set of plume rise equations which have become widely known as "the Briggs equations".
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).
Furthermore, the AREA subtype is best suited for low-level releases with no plume rise (U.S. EPA 1995).
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