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Kevin Kwong and Tyler Szwarc Volcano Power

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Presentation on theme: "Kevin Kwong and Tyler Szwarc Volcano Power"— Presentation transcript:

1 Kevin Kwong and Tyler Szwarc Volcano Power http://www.volcano.si.edu/world/find_regions.cfm

2 Volcano Power Total energy = movement of volcanic material + energy lost due to cooling of ejected material Movement of Molten Material Cooling of Erupted Material Crust Mantle Rising Ash Plume

3 Movement of Volcanic Material Change in potential energy of lava and ash E lava = m g h m = 1.16x10 13 kg/yr g = 9.8 m/s 2 h = 35 km for continental, 10 km for oceanic 3 oceanic eruptions per continental P lava = 3.15*10 10 W Crust Mantle Ash Lava

4 Movement of Volcanic Material Change in potential energy of lava and ash E ash = m g h m = 6.5*10 10 kg/yr g = 9.8 m/s 2 h = 45 km P ash = 9.1 *10 8 W P total material = 3.25 *10 10 W Crust Mantle Ash Lava

5 Heat released and total energy m= (Volume of Lava= 4x10 9 m 3 /yr)*(Density of Lava=2.9x10 3 kg/m 3 ) = 1.16x10 13 kg/yr c= 1700 J/ kg °C T= 1200°C - 100°C = 1100°C L= 560 J/g P= 7.07 x 10 11 Watts P= P lava + P ash + P Q =7.40 x 10 11 Watts Crust Mantle Ash Lava


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