1. Force
2. Mass
3. Acceleration
4. Force = mass ´ acceleration
F = m ´ a
1 Newton: unit of force that will impart an acceleration of 1 m/sec/sec to a mass of 1 kg
1 N = 1 kg m/sec/sec
weight = mass ´ acceleration due to gravity
W = m ´ g
1. Forces acting on a block at rest
normal force = N
weight = W
resultant force = R
2. Addition of a force from the side
a. shear force = T
b. angle of internal friction, f
c. resultant force is proportional to:
normal force, and
coefficient of friction = tanf
R = N tanf
d. just before motion occurs:
T = R
N = W
T = R = W tanf
3. Stress: force per unit area = F/A
a. shear stress,
b. normal stress,
c. strength: frictional shear strength = S
(1) function of:
friction, and
normal force
(2) just before motion occurs, T=R
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4. Summary
N = normal force
W = weight; N=W
T = shear force
R = resultant force or friction force
f = angle of internal friction
R = T = N tanf = W tanf
s = normal stress = N/A = W/A
t = shear stress = T/A
S = shear strength = s tanf
1. Gravity: resolves into two components
N = normal force
T = shear force
magnitude of N & T are a function of slope angle, q
2. Weight = force due to gravity
N = W cosq
T = W sinq
W = volume ´ unit specific weight of material (kg/m3)
(1) volume = B ´ Wd ´ H
(2) g = unit specific weight
(3) W = B ´ Wd ´ H ´ g
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B=base N=normal force
H=height W=weight (force due to gravity)
Wd=width T=shear force
q =slope angle R=resultant force3. Normal stress = s
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4. Shear stress = t
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5. Shear strength, S = s ´ tanf
1. Same forces, different calculations
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a. volume = b ´ h ´ Wd
b. area of contact = B ´ Wd
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area of contact =
2. N = W ´ cosq
3. T = W ´ sinq
4. W = b ´ h ´ Wd ´ g
5.
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6.
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7. S = s ´ tanf
= h ´ g ´ cos2q ´ tanf
8. Pore pressure and cohesion
a. pore pressure = m
m = gw x m x h cos2q
gw = unit specific weight of water
m = fraction of height thats saturated;
0 £ m £ 1
b. effective normal stress
s' = s - m
c. cohesion: increases shear strength
S = stanf
S = c + s'tanf
F = sum of resisting forces/sum of driving forces
F = shear strength/shear stress = S/t
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1. Changes in slope gradient
2. Excessive loading
3. Shocks and vibrations
4. Changes in water content
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©
K.A. Lemke (klemke@uwsp.edu)
Last modified November 24, 2002 |