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Research and Development  599

                 An excellent contribution to improved understanding of  the nature of  laminar dust
               James was given by Dahoe, Hanjalic, and Scarlett (2002). They used a burner appara-
               tus to produce stable cornstarch flames in air, and the laminar burning velocity was
               measured by laser-doppler anemometry. It was found that the laminar burning velocity
               varied with flame shape, and this was accounted for by introducing the “Markstein
               length” of a dusthir flame. This parameter is specific for any given dust cloud. It has a
               magnitude on the order of  the laminar flame thickness of  that specific dust cloud and
               serves as a measure of the sensitivity of the laminar burning velocity to changes in the
               flame shape. Dahoe et al. emphasized that neither the theoretical derivation nor the
               experimental determination of the Markstein length is trivial and much remains to be
               learned about its precise dependence on the chemical and physical properties of the spe-
               cific combustible mixture being investigated. In the light of this work, time seems ripe
               for reconsideringsome conclusionsdrawn from earlier work to determinelaminarbum-
               ing velocities of dust clouds in vertical tube experiments (see Section 4.2.3 in Chapter 4).
               As pointed out by Dahoe et al., buoyancy may have contributed significantly to the
               upward movement of the flame front in these tubes. Also, the observation of a constant
               shape (often about hemispherical) of the upward propagating flame seems to contradict
               the assumptionof a constantburning velocity perpendicular to the flame surfaceimplied
               in the mathematicalcorrection formula frequently used to transform the observed flame
               velocity into the corresponding velocity of a plane laminar flame.

               9.2.4.3
               Limiting Dust Cloud Compositions for Flame Propagation
               This is an important fundamental research topic for at least three different practical
               applications. The first is assessment of  explosive or nonexplosive; the second, assess-
               ment of minimum explosive dust concentration; and the third, assessment of maximum
               permissible oxygen concentration for inerting. Work up to 1990is discussed in Section
               4.2.6 in Chapter 4 and Section 7.13 in Chapter 7. Recent work on some aspects of
               experimental determination of  limiting cloud compositions for flame propagation is
               reviewed in Section 9.4.4.
                 Mintz (1993) found evidence for the existence of  a maximum explosive dust con-
               centration  for dust clouds under certain circumstances. For  a narrow size fraction
               (106-125  pm) of  maize starch, a reasonably well-defined limit of  800-1000  g/m3was
               found. The results were interpreted in terms of a simple “oxygen depletion” model.
                 The influence of particle size distribution on the minimum explosive dust concentra-
               tion was investigated by Poletaev and Korolchenko (1993),using data from experiments
               with polysized polyethylene dusts. Promising agreementbetween theory and experiments
               was obtained. Hanai et al. (1996) measured the minimum explosive dust concentration
               for PMMA particles in air under microgravity conditions. In the absence of buoyancy,
               using a point ignition source, spherical flame ball development was obtained. In the
               range of particle diameters studied,the minimum explosivedust concentration increased
               systematically with the particle diameter. Results from comparative experiments at
               normal gravity differed only modestly from the correspondingmicrogravity results.
                 Hertzberg, Zlochower, and Cashdollar (19924 measured minimum explosive con-
               centrations, maximum explosion pressures and maximum rates of pressure rise at con-
               stant volume, and maximum flame temperatures for clouds in air of dusts of 14 metals.
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