Flame propagation over methane hydrate in an axisymmetric geometry with a non-uniform initial surface temperature profile is investigated experimentally. The methane hydrate in a container with 100 mm diameter and 10 mm depth is ignited at the center of the hydrate surface by a pilot flame. The ignition temperature,
Ts,
ig, which is measured by a thermocouple 1 mm beneath the hydrate surface at the center of the hydrate, is varied from 173K to 253K. When
Ts,
ig, = 173 K, which is lower than the nominal equilibrium temperature of methane hydrate (193 K), the flame propagates axisymmetrically at a low velocity of around 10 mm/s. As the flame propagates, the heat from the flame front dissociates the hydrate. As
Ts,
ig exceeds the nominal equilibrium temperature (
Ts,
ig = 193 and 213 K), the flame propagates at a high velocity of around 1000 mm/s. The hydrate surface dissociates and a methane-air mixture within the flammability limit is formed before ignition, and the flame propagates in the mixture after ignition. At
Ts,
ig = 233 K, the flame propagates fast at around 1000 mm/s until the flame front reaches the radial distance r about 40 mm and the propagation velocity drops to around 10 mm/s and propagates to 50 mm, where it reaches the container wall. The methane hydrate dissociates and methane is ejected into the air up to
r = 40 mm. However, in the region between
r = 40 and 50 mm, the surface temperature is around 253 K where the hydrate is under the self-preservation conditions. At
Ts,
ig of 253 K, the initial temperature is in the self-preservation region, and then the flame propagation velocity is as low as that at
Ts,
ig = 173 K.
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