5. What is Soil Liquefaction
A phenomenon whereby a saturated or
partially saturated soil substantially
loses strength and stiffness in response
to an applied stress, usually
earthquake shaking or other sudden
change in stress condition, causing it
to behave like a liquid.
6. When does it occurs
When the effective stress of
soil is reduced to essentially
zero, which corresponds to a
complete loss of shear strength
8. When does it Occurs
Liquefaction occurring beneath buildings
and other structures can cause major
damage during earthquakes.
Liquefaction occurs in cohesion less soils
(typically those with a higher content of
larger grains such as sand sized) which have
water in the pore spaces, and are poorly
drained.
9. How It Works
When the seismic waves pass through the soil, the
vibrations cause the individual grains in the soil to
move around and
re-adjust their positions
This ultimately results in a decrease in volume of the
soil mass as
the grains pack more tightly together
a reduction in porosity
10. How It Works
The pore water which was originally in those
spaces becomes compressed.
o increase in pore water pressure.
The pore water pressure becomes so high, that
the soil grains become almost Floats
o causing a significant drop in the shear strength