Utilisateur
Porosity
Void Ratio
None of the Above
0 < n < 100
0 ≤ n ≤ 100
0 ≤ S ≤ 100
0 ≤ S ≤ 100
Mixture of sand, silt, and clay size particles in approximately equal proportions
Archimedes' Principle
The unaggregated and uncemented deposits of minerals and organic particles covering the earth's crust
Proportional to the tangent of the angle of shearing resistance
Directly proportional to the square of depth
unstable equilibrium
center of the gravity of the floating body and the metacenter
all of the above
does not vary on any other planet
uncemented aggregate
specific weight
100 to 200
25 to 50
0 to 25
Equal increase in pore water pressure and total stress
Decreases both voids ratio and permeability
Strain to stress
above center of gravity
unstable equilibrium
center of gravity of the floating body and the metacenter
specific weight
water hammer
hydraulic jump
viscosity
1/2
neutral equilibrium
surface tension
All planes except the horizontal and vertical planes
Vane shear test
All of the above
velocity head
b
turbulent flow
steady flow
uniform flow
laminar flow
continuous flow
critical flow
incompressible flow
rotational flow