Lecture 2 - Rheology of magmas Flashcards

1
Q

Controls of viscosity

A

Temperature, composition and gas content

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2
Q

Network formers and breakers

A

Network formers increase viscosity (primarily SiO2)
Network breakers decrease the viscosity (Fe, Mg, Ca)

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3
Q

What determines the viscosity of lava?

A

Linking of (SiO4)4- tetrahedral
Linkages through the O atoms
Increasing silica increases linkages
Additions of cations (Ca, Na) reduce linkages

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4
Q

What does water do to lava?

A

Breaks up silica by adding an oxygen and a new terminus

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5
Q

Rhylote lava compared to basalt

A

Rhyolite is much more viscous

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6
Q

What happens as magma ascends a volcano?

A
  • Decompression - the pressure exerted on it decreases
  • Loss of H20 - the drop in pressure allows water that is dissolved to form steaming bubbles
  • Viscosity increases - bubbles increase the viscosity
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7
Q

How can bubbles can increase or decrease the viscosity of magma?

A

High viscosity - due to flow around spherical or slightly deformed bubbles
Low viscosity - due to the reduced volume fraction of viscous fluid due to presence of bubbles.

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8
Q

How do crystals affect magma viscosity?

A

Adding solid particles of any shape always increases magma viscosity.
No slip at the crystal boundary.

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