Lecture 2 Rheology Flashcards
What is viscosity of magma?
- viscosity is a fluid’s internal resistance to flow
- A measure of the consistency of a substance
logarithmic scale - much more aggressive towards the RHS
Classification by silica content (trend for named silica melts)
increased silica = mire viscous
less iron and magnesium and decrease temperature
least Si02
Basalt 42-52 (also hottest)
Andesite 52-63
Dacite 63-68
Rhyolite more than 68 = silica rich (coldest)
why is there a viscosity trend for silica and iron and magnesium?
silica = (SiO4)4-, si is linked to all 0 atoms making it most viscous, the more silica the more linkages.
- positive cations interact with negative OH- anions to break apart the bonds.
adding cations like iron, magnesium, calcium reduces these linkages.
what does temperature do to viscosity?
lower temperatures = more linkages (bonds) = more viscous.
chemical composition of the magma os a fundamental control on…
its viscosity and its explosivity
What happens as magma physically ascends?
there is decompression and loss of water (H20) into the bubbles and viscosity increases.
bubble shape related to viscosity
Relatively high viscosity - due to flow around spherical or slightly deformed bubbles.
(round shape)
Relatively low viscosities from reduced volume fraction of viscous fluid due to presence of bubbles
free slip surfaces
(thin bubble)
gas content and explosivity
high viscosity inhibits escape of expanding bubbles leading to pressure build up while magma is ascending.
crystals and viscosity
whenever solid is added it increases magma viscosity.
different from bubbles as there is no slip at the crystal boundary.
more crystals always = higher viscosity.
what’s the link between basalt surface morphology and crystal content?
pahoehoe = less crystals and a a = more crystal content
pressure and viscosity
viscosity decreases when pressure increases
Temperature and viscosity
- viscosity increases significantly on cooling
(partly due to crystallization)
Volatile Content and viscosity
- viscosity lower with increasing volatile content
- water depolymerizes melt by breaking Si–O–Si bond
Crystal Content and viscosity
- suspended crystals increase the bulk viscosity
Bubble Content and viscosity
- basalts - little effect
- rhyolite - big effect