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Soil Dynamics
2. Dynamics of Discrete Systems
Cristian Soriano Camelo1
1Federal University of Rio de Janeiro
Geotechnical Engineering
July 06th, 2017
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 1 / 35
Outline
1 Introduction
Dynamics of Discrete Systems
2 Vibrating systems
Categories, Degrees of freedom
3 Single Degree of Freedom Systems (SDOF)
Definition, equations of motion, response
4 Damping
Viscous damping, Other measures of energy dissipation
5 Multiple Degree of Freedom Systems
Equations of motion
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 2 / 35
Outline
1 Introduction
Dynamics of Discrete Systems
2 Vibrating systems
Categories, Degrees of freedom
3 Single Degree of Freedom Systems (SDOF)
Definition, equations of motion, response
4 Damping
Viscous damping, Other measures of energy dissipation
5 Multiple Degree of Freedom Systems
Equations of motion
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 3 / 35
Introduction
Vibrating systems
Discrete elements:
spring and masses
Dynamic response
of discrete systems
Dynamics of discrete systems: simple systems, damping, base motion
and nonlinearity.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 4 / 35
Outline
1 Introduction
Dynamics of Discrete Systems
2 Vibrating systems
Categories, Degrees of freedom
3 Single Degree of Freedom Systems (SDOF)
Definition, equations of motion, response
4 Damping
Viscous damping, Other measures of energy dissipation
5 Multiple Degree of Freedom Systems
Equations of motion
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 5 / 35
Vibrating systems
Rigid systems: No strains occur → all points move in the same phase
(i.e rigid body).
Compliant systems: different points within the system may move
differently (and out of phase).
Soils and structures are studied in terms of compliant systems:
structural dynamics and earthquake engineering.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 6 / 35
Vibrating systems
Compliant systems can me characterized by the distribution of their
mass:
Discrete systems:The mass concentrated in a finite number of
locations.
Continuous systems: the mass is distributed throughout the system.
Those concepts results in the dynamic degrees of freedom that describe
the position of all the significant masses of the system.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 7 / 35
Outline
1 Introduction
Dynamics of Discrete Systems
2 Vibrating systems
Categories, Degrees of freedom
3 Single Degree of Freedom Systems (SDOF)
Definition, equations of motion, response
4 Damping
Viscous damping, Other measures of energy dissipation
5 Multiple Degree of Freedom Systems
Equations of motion
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 8 / 35
Single Degree of Freedom Systems
SDOF:Discrete systems whose position can be described by a single
variable. The degrees of freedom can be a translational displacement or
a rotational displacement.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 9 / 35
Equation of motion - SDOF
External load Q(t), inertial force fi, viscous damping force fD and
elastic spring force fS.
- In terms of equilibrium:fi(t) + fD(t) + fS(t) = Q(t)
- In terms of motion of the mass: md2u(t)
dt2 + cdu
dt + ku(t) = Q(t)
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 10 / 35
Equation of motion - Base shaking
In earthquake engineering problems, dynamic loading often results
from vibration of the supports of a system rather than from dynamic
external loads.
Equation of motion: mu′′(t) + cu′(t) + ku = 0
Substituting: u′′
t (t) = u′′
b (t) + u′′(t) →mu′′ + cu′ + ku = −mu′′
b
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 11 / 35
Response of linear SDOF systems
Forced vibration: when the mass is subjected to loading.
Free vibration:absence of external loading or base shaking.
Undamped free vibrations c=0 Q(t)=0
Damped free vibrations c>0 Q(t)=0
Undamped forced vibrations c=0 Q(t)=0
Damped forced vibrations c>0 Q(t)=0
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 12 / 35
Undamped free vibrations
No external load is considered, c=0.
u =
u′
0
ω0
sin(ω0t) + u0cos(ω0t)
Where ω0 = k
m is the undamped natural circular frequency.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 13 / 35
Undamped free vibrations
Example 1: An undamped oscillator has a mas m (5 and 2)kg,
k=45N/m. At time t=0, the oscillator is given an initial position
x0=2m and an initial velocity v0=4m/s.
equat(m , b , k , x0 , v0 ):= {bx′(t) + kx(t) + mx′′(t) = 0, x(0) = x0, x′(0) = v0}
response(m , b , k , x0 , v0 ):=x(t)/. Flatten[DSolve[equat(m, b, k, x0, v0), x(t), t]]
x2(t ) = response(m, 0, 45, 2, 4) = 2
15
2
√
5
√
m sin 3
√
5t√
m
+ 15 cos 3
√
5t√
m
1 2 3 4 5
t(s)
-2
-1
1
2
x1(meters)
Undamped Vibration Example
1 2 3 4 5
t(s)
-2
-1
1
2
x1(meters)
Undamped Vibration Example
m=5 kg m=2kg
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 14 / 35
Damped free vibrations
In real systems, energy may be lost as a result of friction, heat
generation, air resistance or other physical mechanisms. Hence the free
vibration response of a SDOF system will diminish with time. For
damped free vibrations:
mu′′ + cu′ + ku = 0
Where ξ is the damping ratio.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 15 / 35
Damped free vibrations
Example 2: The structure shown in the figure is released from an
initial displacement of 1 cm with an initial velocity of -5cm/s.
Compute the time history of response of the mass.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 16 / 35
Damped free vibrations
x3(t ) = response(1000, 1000, 20000, 0.01, −0.05)
0.01e− t
2 1. cos
√
79t
2 − 1.01258 sin
√
79t
2
2 4 6 8
Time(s)
-0.010
-0.005
0.005
0.010
Diplacement(m)
Displacement response
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 17 / 35
Damped forced vibrations
The equation of motion for a damped SDOF system subjected to
harmonic loading of the form Q(t) = Q0sin(ωt) is:
mu′ + cu′ + ku = Q0sin(ωt)
The solution of the equation indicates that the response has two
components. One component occurs in response occurs at the natural
frequency of the system ω0 and other at the natural frequency of the
loading ω.
u = Q0
k
1
1−β2 (sin(ωt) + βsin(ω0t))
Where β = ω
ω0
, tuning ratio.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 18 / 35
Undamped forced vibrations
The relationship 1
1−β2 can be thought as the amount by which the
static displacement amplitude is magnified by the harmonic load.
Note that for loading frequencies lower than
√
2ω0 the displacement
amplitude is greater than the static displacement.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 19 / 35
Undamped forced vibrations
Example 3: Simulation of an undamped SDOF system subjected to
different excitation frequencies: twice lower than the natural frequency,
twice higher than the natural frequency and at natural frequency.
Natural angular frequency ω0 4.5 Hz
Damping ratio 0
Driving amplitude 100 kN
Driving angular frequency 2.25 Hz, 9 Hz, 4.5 Hz
Mass (m) 6500 kg
k = (2πω2
0)m 5200000 N/m
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 20 / 35
Undamped forced vibrations
Case 1: ω = ω0/2
Case 2: ω = 2ω0
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 21 / 35
Undamped forced vibrations
Case 3: ω = ω0
It can be seen that the response grows without bound indicating resonance of the system,
the corresponding frequency is called resonance frequency.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 22 / 35
Damped forced vibrations
The most general case is a damped system subjected to forced
harmonic loading. The general equation of a damped SDOF system
subjected to harmonic loading of the form Q(t) = Q0sin(ωt) is:
mu′′ + cu′ + ku = Q0sin(ωt)
Example 4: Simulation of a resonant damped SDOF system
subjected to an excitation frequency twice lower than the natural
frequency and different damping ratios ξ = 0.1, 0.3.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 23 / 35
Damped forced vibrations
Case 1: ξ = 0.1
Case 2: ξ = 0.3
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 24 / 35
Outline
1 Introduction
Dynamics of Discrete Systems
2 Vibrating systems
Categories, Degrees of freedom
3 Single Degree of Freedom Systems (SDOF)
Definition, equations of motion, response
4 Damping
Viscous damping, Other measures of energy dissipation
5 Multiple Degree of Freedom Systems
Equations of motion
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 25 / 35
Damping
Viscous Damping:The most commonly used mechanism for
representing energy dissipation. For a viscous SDOF system subjected
to a harmonic displacement u(t) = u0sin(ωt):
F(t) = ku(t) + cu′(t) = ku0sin(ωt) + cωu0cos(ωt)
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 26 / 35
Damping
Evaluating these functions from a time t0 to time t0 + 2π
ω , yields the
force-displacement values for one cycle of a hysteresis loop.
When viscous damping c = 0 there is a linear elastic-stress relationship.
For nonzero damoing, the hysteresis loop becomes elliptical.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 27 / 35
Damping
The energy dissipated in one cycle of oscillation is:
WD =
t0+ 2π
ω
t0
F du
dt dt = πcωu2
0
At maximum displacement, the velocity is zero and the energy stored
in the system is:
Ws = 1
2 ku2
0
And the damping ratio is given by: ξ = WD
4πWS
This expression is used for graphical determination of the damping
ratio.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 28 / 35
Response spectra
The response spectrum describes the maximum response of a SDOF
system to a particular input motion as a function of the natural
frequency (or natural period) and damping ratio. The response may be
expressed in terms of acceleration, velocity or displacement.
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 29 / 35
Response spectra
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 30 / 35
Response spectra
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 31 / 35
Outline
1 Introduction
Dynamics of Discrete Systems
2 Vibrating systems
Categories, Degrees of freedom
3 Single Degree of Freedom Systems (SDOF)
Definition, equations of motion, response
4 Damping
Viscous damping, Other measures of energy dissipation
5 Multiple Degree of Freedom Systems
Equations of motion
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 32 / 35
Multiple Degree of Freedom Systems
In systems in which the motion cannot
be described by a single variable
(buildings, bridges, other structures).
Equations of motion:
[m]u”+[c]u’+[k]u=q(t)
Example 5: Determine the Equations of Motion of the two degrees of
freedom system shown in the figure.
m1=2 m2=1 c1=0.1 c2=0.3
k1=6 k2=3 p1=2sin(3t) p2=5cos(2t)
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 33 / 35
Multiple Degree of Freedom Systems
2 0
0 1
u1”
u2”
+
0.4 −0.3
−0.3 0.3
u1’
u2’
+
9 −3
−3 3
u1
u2
=
2sin3t
5cos2t
m=
2 0
0 1
; c=
0.4 −0.3
−0.3 0.3
; k=
9 −3
−3 3
u1
u2
; q=
2sin3t
5cos2t
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 34 / 35
For Further Reading I
Steven L. Kramer.
Geotechnical Earthquake Engineering.
Prentice Hall, 1996.
http://www.strongmotioncenter.org/
Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 35 / 35

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Soil dyn __2

  • 1. Soil Dynamics 2. Dynamics of Discrete Systems Cristian Soriano Camelo1 1Federal University of Rio de Janeiro Geotechnical Engineering July 06th, 2017 Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 1 / 35
  • 2. Outline 1 Introduction Dynamics of Discrete Systems 2 Vibrating systems Categories, Degrees of freedom 3 Single Degree of Freedom Systems (SDOF) Definition, equations of motion, response 4 Damping Viscous damping, Other measures of energy dissipation 5 Multiple Degree of Freedom Systems Equations of motion Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 2 / 35
  • 3. Outline 1 Introduction Dynamics of Discrete Systems 2 Vibrating systems Categories, Degrees of freedom 3 Single Degree of Freedom Systems (SDOF) Definition, equations of motion, response 4 Damping Viscous damping, Other measures of energy dissipation 5 Multiple Degree of Freedom Systems Equations of motion Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 3 / 35
  • 4. Introduction Vibrating systems Discrete elements: spring and masses Dynamic response of discrete systems Dynamics of discrete systems: simple systems, damping, base motion and nonlinearity. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 4 / 35
  • 5. Outline 1 Introduction Dynamics of Discrete Systems 2 Vibrating systems Categories, Degrees of freedom 3 Single Degree of Freedom Systems (SDOF) Definition, equations of motion, response 4 Damping Viscous damping, Other measures of energy dissipation 5 Multiple Degree of Freedom Systems Equations of motion Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 5 / 35
  • 6. Vibrating systems Rigid systems: No strains occur → all points move in the same phase (i.e rigid body). Compliant systems: different points within the system may move differently (and out of phase). Soils and structures are studied in terms of compliant systems: structural dynamics and earthquake engineering. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 6 / 35
  • 7. Vibrating systems Compliant systems can me characterized by the distribution of their mass: Discrete systems:The mass concentrated in a finite number of locations. Continuous systems: the mass is distributed throughout the system. Those concepts results in the dynamic degrees of freedom that describe the position of all the significant masses of the system. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 7 / 35
  • 8. Outline 1 Introduction Dynamics of Discrete Systems 2 Vibrating systems Categories, Degrees of freedom 3 Single Degree of Freedom Systems (SDOF) Definition, equations of motion, response 4 Damping Viscous damping, Other measures of energy dissipation 5 Multiple Degree of Freedom Systems Equations of motion Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 8 / 35
  • 9. Single Degree of Freedom Systems SDOF:Discrete systems whose position can be described by a single variable. The degrees of freedom can be a translational displacement or a rotational displacement. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 9 / 35
  • 10. Equation of motion - SDOF External load Q(t), inertial force fi, viscous damping force fD and elastic spring force fS. - In terms of equilibrium:fi(t) + fD(t) + fS(t) = Q(t) - In terms of motion of the mass: md2u(t) dt2 + cdu dt + ku(t) = Q(t) Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 10 / 35
  • 11. Equation of motion - Base shaking In earthquake engineering problems, dynamic loading often results from vibration of the supports of a system rather than from dynamic external loads. Equation of motion: mu′′(t) + cu′(t) + ku = 0 Substituting: u′′ t (t) = u′′ b (t) + u′′(t) →mu′′ + cu′ + ku = −mu′′ b Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 11 / 35
  • 12. Response of linear SDOF systems Forced vibration: when the mass is subjected to loading. Free vibration:absence of external loading or base shaking. Undamped free vibrations c=0 Q(t)=0 Damped free vibrations c>0 Q(t)=0 Undamped forced vibrations c=0 Q(t)=0 Damped forced vibrations c>0 Q(t)=0 Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 12 / 35
  • 13. Undamped free vibrations No external load is considered, c=0. u = u′ 0 ω0 sin(ω0t) + u0cos(ω0t) Where ω0 = k m is the undamped natural circular frequency. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 13 / 35
  • 14. Undamped free vibrations Example 1: An undamped oscillator has a mas m (5 and 2)kg, k=45N/m. At time t=0, the oscillator is given an initial position x0=2m and an initial velocity v0=4m/s. equat(m , b , k , x0 , v0 ):= {bx′(t) + kx(t) + mx′′(t) = 0, x(0) = x0, x′(0) = v0} response(m , b , k , x0 , v0 ):=x(t)/. Flatten[DSolve[equat(m, b, k, x0, v0), x(t), t]] x2(t ) = response(m, 0, 45, 2, 4) = 2 15 2 √ 5 √ m sin 3 √ 5t√ m + 15 cos 3 √ 5t√ m 1 2 3 4 5 t(s) -2 -1 1 2 x1(meters) Undamped Vibration Example 1 2 3 4 5 t(s) -2 -1 1 2 x1(meters) Undamped Vibration Example m=5 kg m=2kg Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 14 / 35
  • 15. Damped free vibrations In real systems, energy may be lost as a result of friction, heat generation, air resistance or other physical mechanisms. Hence the free vibration response of a SDOF system will diminish with time. For damped free vibrations: mu′′ + cu′ + ku = 0 Where ξ is the damping ratio. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 15 / 35
  • 16. Damped free vibrations Example 2: The structure shown in the figure is released from an initial displacement of 1 cm with an initial velocity of -5cm/s. Compute the time history of response of the mass. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 16 / 35
  • 17. Damped free vibrations x3(t ) = response(1000, 1000, 20000, 0.01, −0.05) 0.01e− t 2 1. cos √ 79t 2 − 1.01258 sin √ 79t 2 2 4 6 8 Time(s) -0.010 -0.005 0.005 0.010 Diplacement(m) Displacement response Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 17 / 35
  • 18. Damped forced vibrations The equation of motion for a damped SDOF system subjected to harmonic loading of the form Q(t) = Q0sin(ωt) is: mu′ + cu′ + ku = Q0sin(ωt) The solution of the equation indicates that the response has two components. One component occurs in response occurs at the natural frequency of the system ω0 and other at the natural frequency of the loading ω. u = Q0 k 1 1−β2 (sin(ωt) + βsin(ω0t)) Where β = ω ω0 , tuning ratio. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 18 / 35
  • 19. Undamped forced vibrations The relationship 1 1−β2 can be thought as the amount by which the static displacement amplitude is magnified by the harmonic load. Note that for loading frequencies lower than √ 2ω0 the displacement amplitude is greater than the static displacement. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 19 / 35
  • 20. Undamped forced vibrations Example 3: Simulation of an undamped SDOF system subjected to different excitation frequencies: twice lower than the natural frequency, twice higher than the natural frequency and at natural frequency. Natural angular frequency ω0 4.5 Hz Damping ratio 0 Driving amplitude 100 kN Driving angular frequency 2.25 Hz, 9 Hz, 4.5 Hz Mass (m) 6500 kg k = (2πω2 0)m 5200000 N/m Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 20 / 35
  • 21. Undamped forced vibrations Case 1: ω = ω0/2 Case 2: ω = 2ω0 Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 21 / 35
  • 22. Undamped forced vibrations Case 3: ω = ω0 It can be seen that the response grows without bound indicating resonance of the system, the corresponding frequency is called resonance frequency. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 22 / 35
  • 23. Damped forced vibrations The most general case is a damped system subjected to forced harmonic loading. The general equation of a damped SDOF system subjected to harmonic loading of the form Q(t) = Q0sin(ωt) is: mu′′ + cu′ + ku = Q0sin(ωt) Example 4: Simulation of a resonant damped SDOF system subjected to an excitation frequency twice lower than the natural frequency and different damping ratios ξ = 0.1, 0.3. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 23 / 35
  • 24. Damped forced vibrations Case 1: ξ = 0.1 Case 2: ξ = 0.3 Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 24 / 35
  • 25. Outline 1 Introduction Dynamics of Discrete Systems 2 Vibrating systems Categories, Degrees of freedom 3 Single Degree of Freedom Systems (SDOF) Definition, equations of motion, response 4 Damping Viscous damping, Other measures of energy dissipation 5 Multiple Degree of Freedom Systems Equations of motion Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 25 / 35
  • 26. Damping Viscous Damping:The most commonly used mechanism for representing energy dissipation. For a viscous SDOF system subjected to a harmonic displacement u(t) = u0sin(ωt): F(t) = ku(t) + cu′(t) = ku0sin(ωt) + cωu0cos(ωt) Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 26 / 35
  • 27. Damping Evaluating these functions from a time t0 to time t0 + 2π ω , yields the force-displacement values for one cycle of a hysteresis loop. When viscous damping c = 0 there is a linear elastic-stress relationship. For nonzero damoing, the hysteresis loop becomes elliptical. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 27 / 35
  • 28. Damping The energy dissipated in one cycle of oscillation is: WD = t0+ 2π ω t0 F du dt dt = πcωu2 0 At maximum displacement, the velocity is zero and the energy stored in the system is: Ws = 1 2 ku2 0 And the damping ratio is given by: ξ = WD 4πWS This expression is used for graphical determination of the damping ratio. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 28 / 35
  • 29. Response spectra The response spectrum describes the maximum response of a SDOF system to a particular input motion as a function of the natural frequency (or natural period) and damping ratio. The response may be expressed in terms of acceleration, velocity or displacement. Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 29 / 35
  • 30. Response spectra Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 30 / 35
  • 31. Response spectra Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 31 / 35
  • 32. Outline 1 Introduction Dynamics of Discrete Systems 2 Vibrating systems Categories, Degrees of freedom 3 Single Degree of Freedom Systems (SDOF) Definition, equations of motion, response 4 Damping Viscous damping, Other measures of energy dissipation 5 Multiple Degree of Freedom Systems Equations of motion Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 32 / 35
  • 33. Multiple Degree of Freedom Systems In systems in which the motion cannot be described by a single variable (buildings, bridges, other structures). Equations of motion: [m]u”+[c]u’+[k]u=q(t) Example 5: Determine the Equations of Motion of the two degrees of freedom system shown in the figure. m1=2 m2=1 c1=0.1 c2=0.3 k1=6 k2=3 p1=2sin(3t) p2=5cos(2t) Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 33 / 35
  • 34. Multiple Degree of Freedom Systems 2 0 0 1 u1” u2” + 0.4 −0.3 −0.3 0.3 u1’ u2’ + 9 −3 −3 3 u1 u2 = 2sin3t 5cos2t m= 2 0 0 1 ; c= 0.4 −0.3 −0.3 0.3 ; k= 9 −3 −3 3 u1 u2 ; q= 2sin3t 5cos2t Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 34 / 35
  • 35. For Further Reading I Steven L. Kramer. Geotechnical Earthquake Engineering. Prentice Hall, 1996. http://www.strongmotioncenter.org/ Cristian Soriano Camelo (UFRJ) Soil Dynamics July 06th, 2017 35 / 35