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U.S. Department of Energy
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Physical modeling of heavy plume dispersion

Thesis/Dissertation ·
OSTI ID:6678869
An LNG vapor plume at boiloff conditions is heavier than air. Although the plume will eventually become positively buoyant due to heat absorbed from the surroundings, much of the dispersion will occur while the plume density is greater than that of air. In laboratory tests, dispersion during the heavier-than-air phase was approximated by means of isothermal-model plumes produced by high-molecular-weight gases. These heavy gases were introduced into a wind tunnel via an area source mounted flush on the wind-tunnel floor. Concentration sensors downwind of this source were used to measure the structure of the different model plumes tested. Methods for scaling between model tests and field scale events are defined. The concentration scaling theory used by previous investigators was found to cause large errors and a new theory was developed. An extensive data base on the structure of different laboratory heavy plumes was obtained. These experiments included a large range of conditions for source gas specific gravity, gas flow rate and wind speed. Three different procedures were formulated whereby a single model test can be predictive of a larger class of field events. These enhanced scaling procedures are analyzed with respect to the measured laboratory data base to assist in specification of their capabilities and limitations. A useful empirical description of all the continuous plume tests was developed, and its applicability to field conditions discussed. Model tests on measured field scale LNG spills were performed to validate physical modeling capabilities. When the model tests reproduced the approach flow wind characteristics properly the plume concentration field was in good agreement with the field test results.
Research Organization:
Colorado State Univ., Fort Collins, CO (USA)
OSTI ID:
6678869
Country of Publication:
United States
Language:
English