Mixing of a Point Source Pollutant by Natural Convection Flow within a Room

A. V. Baughman, Ashok Gadgil, William W. Nazaroff

Indoor Air · 1994 · 95 citations · 3 references

Concepts

TL;DR

Indoor air quality models often assume instantaneous, complete mixing, which is inappropriate for situations such as segregating smokers to protect nonsmokers from environmental tobacco smoke. This study quantitatively characterizes the dispersion rate of cigarette smoke in a 31‑m³, low air‑exchange room under natural convection. The authors released pulsed tracer gas (SF6/He) above a heated coil, sampled air from 41 locations during each run, analyzed SF6 by GC‑ECD, and repeated the experiments under nearly isothermal, heater‑induced, and solar‑radiation convection conditions. Mixing times ranged from 7–10 minutes under solar‑radiation convection to 80–100 minutes under nearly isothermal conditions.

Abstract

Indoor air quality models are commonly based on the assumption of instantaneous and complete air mixing within a zone. Such an assumption is not appropriate for all circumstances, such as investigating the utility of segregating smokers to reduce nonsmoker exposure to environmental tobacco smoke. This experimental study characterizes quantitatively the rate at which smoke from a cigarette disperses within an unoccupied, 31-m3, low air-exchange rate room under natural convection flow conditions. Sidestream smoke from a smoldering cigarette was simulated with a pulsed release of a tracer gas – a neutrally buoyant mixture of sulfur hexafluoride (SF6) in helium – above an electrically heated coil. During each experimental run, sequential air samples were collected remotely, using gas-tight syringes, from 41 locations within the room. After each run, these samples were analyzed for SF6 content using a gas chromatograph with an electron-capture detector. Duplicate runs were conducted under three conditions: nearly isothermal surfaces; convection from a 500–watt heater; and convection from incoming solar radiation. Characteristic mixing times ranged from 7–10 minutes for the solar radiation case to 80–100 minutes for the nearly isothermal case.

References

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