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European Erasmus Mundus Master Course Sustainable Constructions under Natural Hazards and Catastrophic Events 520121-1-2011-1-CZ-ERA MUNDUS-EMMC 2C09 Design for seismic and climate changes Lecture 02: Dynamic response of single-degree-of-freedom systems I Daniel Grecea, Politehnica University of Timisoara 03/04/2014

2C09 Design for seismic and climate changes

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Page 1: 2C09 Design for seismic and climate changes

European Erasmus Mundus Master Course

Sustainable Constructions

under Natural Hazards and Catastrophic Events520121-1-2011-1-CZ-ERA MUNDUS-EMMC

2C09

Design for seismic and climate changes

Lecture 02: Dynamic response of single-degree-of-freedom systems I

Daniel Grecea, Politehnica University of Timisoara

03/04/2014

Page 2: 2C09 Design for seismic and climate changes

L2 – Dynamic response of single-degree-of-freedom systems I

European Erasmus Mundus Master Course

Sustainable Constructions under Natural

Hazards and Catastrophic Events

L2.1 – Introduction to dynamics of structures.

L2.2 – Solutions methods for the equation of motion.

L2.3 – Free vibration analysis of SDOF systems.

2C09-L2 – Dynamic response of single-degree-of-

freedom systems I

Page 3: 2C09 Design for seismic and climate changes

Dynamics of structures

Dynamics of

structures

determination of

response of

structures under

the effect of

dynamic loading

Dynamic load is

one whose

magnitude,

direction, sense

and point of

application changes

in time

t

p(t)

p(t)

p(t)

t

t

t

üg(t)

Page 4: 2C09 Design for seismic and climate changes

Single degree of freedom systems

Simple structures:

– mass m

– stiffness k

Objective: find out response of SDOF system under the

effect of:

– a dynamic load acting on the mass

– a seismic motion of the base of the structure

The number of degree of

freedom (DOF) necessary

for dynamic analysis of a

structure is the number of

independent displacements

necessary to define the

displaced position of

masses with respect to

their initial position

k

m

Single degree of freedom

systems (SDOF)

Page 5: 2C09 Design for seismic and climate changes

Single degree of freedom systems

One-storey frame =

– mass component

– stiffness component

– damping component

Number of dynamic degrees of freedom = 1

Number of static degrees of freedom = ?

Page 6: 2C09 Design for seismic and climate changes

Force-displacement relationship

Page 7: 2C09 Design for seismic and climate changes

Force-displacement relationship

Linear elastic system:

– elastic material

– first order analysis

Inelastic system:

– plastic material

– First-order or second-order analysis

Sf k u

,S Sf f u u

Page 8: 2C09 Design for seismic and climate changes

Damping force

Damping: decreasing with time of amplitude of vibrations

of a system let to oscillate freely

Cause: thermal effect of elastic cyclic deformations of the

material and internal friction

Page 9: 2C09 Design for seismic and climate changes

Damping

Damping in real structures:

– friction in steel connections

– opening and closing of microcracks in r.c. elements

– friction between structural and non-structural elements

Mathematical description of these components

impossible

Modelling of damping in real structures

equivalent viscous damping

Page 10: 2C09 Design for seismic and climate changes

Damping

Relationship between damping force

and velocity:

c - viscous damping coefficient

units: (Force x Time / Length)

Determination of viscous damping:

– free vibration tests

– forced vibration tests

Equivalent viscous damping modelling of the energy

dissipated by the structure in the elastic range

Df c u

Page 11: 2C09 Design for seismic and climate changes

Equation of motion for an external force

Newton’s second law of motion

D'Alambert principle

Stiffness, damping and mass components

Page 12: 2C09 Design for seismic and climate changes

Equation of motion: Newton’s 2nd law of motion

Forces acting on mass m:

– external force p(t)

– elastic (or inelastic) resisting force fS

– damping force fD

External force p(t), displacement u(t), velocity and

acceleration are positive in the positive direction of

the x axis

Newton’s second law of motion:

( )u t( )u t

S Dp f f mu

S Dmu f f p

( )mu cu ku p t

Page 13: 2C09 Design for seismic and climate changes

Equation of motion: D'Alambert principle

Inertial force

– equal to the product between force and acceleration

– acts in a direction opposite to acceleration

D'Alambert principle: a system is in equilibrium at each

time instant if al forces acting on it (including the inertia

force) are in equilibrium

I S Df f f p

If mu

S Dmu f f p

( )mu cu ku p t

Page 14: 2C09 Design for seismic and climate changes

Equation of motion:

stiffness, damping and mass components Under the external force p(t), the system state is

described by

– displacement u(t)

– velocity

– acceleration

System = combination of three pure components:

– stiffness component

– damping component

– mass component

External force p(t) distributed to the three components

( )u t

( )u t

If muDf c u

Sf k u

I S Df f f p

Page 15: 2C09 Design for seismic and climate changes

SDOF systems: classical representation

Page 16: 2C09 Design for seismic and climate changes

Equation of motion: seismic excitation

Dynamics of structures in the case of seismic motion

determination of structural response under the effect of

seismic motion applied at the base of the structure

Ground displacement ug

Total (or absolute) displacement of the mass ut

Relative displacement between mass and ground u

( ) ( ) ( )t

gu t u t u t

Page 17: 2C09 Design for seismic and climate changes

Equation of motion: seismic excitation

D'Alambert principle of dynamic equilibrium

Elastic forces relative displacement u

Damping forces relative displacement u

Inertia force total displacement ut

0I S Df f f

Df c u

Sf k u

t

If mu

0tmu cu ku

( ) ( ) ( )t

gu t u t u t

gmu cu ku mu

Page 18: 2C09 Design for seismic and climate changes

Equation of motion: seismic excitation

Equation of motion in the case of an external force

Equation of motion in the case of seismic excitation

Equation of motion for a system subjected to seismic

motion described by ground acceleration is identical

to that of a system subjected to an external force

Effective seismic force

gmu cu ku mu

( )mu cu ku p t

gmugu

( ) ( )eff gp t mu t

Page 19: 2C09 Design for seismic and climate changes

Problem formulation

Fundamental problem in dynamics of structures:

determination of the response of a (SDOF) system under

a dynamic excitation

– a external force

– ground acceleration applied to the base of the structure

"Response" any quantity that characterizes behaviour

of the structure

– displacement

– velocity

– mass acceleration

– forces and stresses in structural members

Page 20: 2C09 Design for seismic and climate changes

Determination of element forces

Solution of the equation of motion of the SDOF system

displacement time history

Displacements forces in structural elements

– Imposed displacements forces in structural elements

– Equivalent static force: an external static force fS that produces

displacements u determined from dynamic analysis

Forces in structural elements by static analysis of the structure

subjected to equivalent seismic forces fS

( )u t

( ) ( )sf t ku t

Page 21: 2C09 Design for seismic and climate changes

Combination of static and dynamic response

Linear elastic systems:

superposition of effects possible

total response can be determined

through the superposition of the

results obtained from:

– static analysis of the structure under

permanent and live loads, temperature

effects, etc.

– dynamic response of the structure

Inelastic systems: superposition of

effects NOT possible dynamic

response must take account of

deformations and forces existing in

the structure before application of

dynamic excitation

Page 22: 2C09 Design for seismic and climate changes

Solution of the equation of motion

Equation of motion of a SDOF system

differential linear non-homogeneous equation of second

order

In order to completely define the problem:

– initial displacement

– initial velocity

Solution methods:

– Classical solution

– Duhamel integral

– Numerical techniques

( ) ( ) ( ) ( )mu t cu t ku t p t

(0)u

(0)u

Page 23: 2C09 Design for seismic and climate changes

Classical solution

Complete solution u(t) of a linear non-homogeneous

differential equation of second order is composed of

– complementary solution uc(t) and

– particular solution up(t)

u(t) = uc(t) +up(t)

Second order equation 2 integration constants initial

conditions

Classical solution useful in the case of

– free vibrations

– forces vibrations, when dynamic excitation is defined analytically

Page 24: 2C09 Design for seismic and climate changes

Classical solution: example

Equation of motion of an undamped (c=0) SDOF system

excited by a step force p(t)=p0, t≥0:

Particular solution:

Complementary solution:

where A and B are integration constants and

The complete solution

Initial conditions: for t=0 we have and

the eq. of motion

0mu ku p 0( )p

pu t

k

( ) cos sinc n nu t A t B t

n k m

0( ) cos sinn n

pu t A t B t

k

(0) 0u (0) 0u

0 0p

A Bk

0( ) (1 cos )n

pu t t

k

Page 25: 2C09 Design for seismic and climate changes

Duhamel integral

Basis: representation of the dynamic excitation as a

sequence of infinitesimal impulses

Response of a system excited by the force p(t) at time t

sum of response of all impulses up to that time

Applicable only to "at rest" initial conditions

Useful when the force p(t)

– is defined analytically

– is simple enough to evaluate analytically the integral

0

1( ) ( )sin[ ( )]

t

n

n

u t p t dm

(0) 0u (0) 0u

Page 26: 2C09 Design for seismic and climate changes

Duhamel integral: example

Equation of motion of an undamped (c=0) SDOF system,

excited by a ramp force p(t)=p0, t≥0:

Equation of motion

0mu ku p

0( ) (1 cos )n

pu t t

k

0 (1 cos )n

pt

k

00

0 0

cos ( )1( ) sin[ ( )]

tt

nn

n n n

p tu t p t d

m m

Page 27: 2C09 Design for seismic and climate changes

Undamped free vibrations

General form of the equation of motion:

Equation of motion in the case of undamped free

vibrations:

Vibrations the system disturbed from the static

equilibrium position by

– initial displacement

– initial velocity

Classical solution

where

( )mu cu ku p t

0mu ku

(0)u

(0)u

(0)( ) (0)cos sinn n

n

uu t u t t

n k m

Page 28: 2C09 Design for seismic and climate changes

Undamped free vibrations

Simple harmonic motion(0)

( ) (0)cos sinn n

n

uu t u t t

Page 29: 2C09 Design for seismic and climate changes

Undamped free vibrations

Natural period of vibration - Tn - time needed for

an undamped SDOF system to perform a

complete cycle of free vibrations

Natural circular frequency

Natural frequency of vibration fn represents the

number of complete cycles performed by the

system in one second

mass stiffness

"Natural" - depends only on the properties of the

SDOF system

2n

n

T

1n

n

fT

2

nnf

n k m

n k m

Page 30: 2C09 Design for seismic and climate changes

Undamped free vibrations

Alternative expressions for n, fn, Tn:

elastic deformation of a SDOF system under

a static force equal to mg

Amplitude: magnitude of oscillations

12

2

stn n n

st st

g gf T

g

st mg k

2

2

0

00

n

uu u

Page 31: 2C09 Design for seismic and climate changes

Damped free vibrations

General form of the eq. of motion:

Equation of motion in the case of damped free vibrations:

Dividing eq. by m we obtain

with the notations:

Critical damping coefficient

Damping coefficient c - a measure of the energy

dissipated in a complete cycle

- critical damping ratio: a non-dimensional measure of

damping, which depends on the stiffness and mass as

well

( )mu cu ku p t

0mu cu ku 22 0n nu u u

n k m 2 n cr

c c

m c

22 2cr n

n

kc m km

Page 32: 2C09 Design for seismic and climate changes

Types of motion

c=ccr or = 1 the system returns to the position of

equilibrium without oscillation

c>ccr or > 1 the system returns to the position of

equilibrium without oscillation, but slower

c<ccr or < 1 the system oscillates with respect to the

equilibrium position with progressively decreasing

amplitudes

Page 33: 2C09 Design for seismic and climate changes

Types of motion

ccr - the smallest value of the damping coefficient that

completely prevents oscillations

Most engineering structures - underdamped (c<ccr)

Few reasons to study:

– critically damped systems (c=ccr)

– overdamped systems (c>ccr)

Page 34: 2C09 Design for seismic and climate changes

Underdamped systems

Solution of the eq. for systems with

c<ccr or < 1:

with the notation:

(0) (0)( ) (0)cos sinnt n

D D

D

u uu t e u t t

0mu cu ku

21D n

Page 35: 2C09 Design for seismic and climate changes

The effect of damping in underdamped systems

Envelope of damped vibrations

Lowering of the circular frequency from n to D

Lengthening of he period of vibration form Tn to TD

nte

2

2 0 (0)0

n

D

u uu

Page 36: 2C09 Design for seismic and climate changes

Attenuation of motion

Ratio between displacement at time t and the one after a

period TD is independent of t:

Using and

( )

exp( )

n D

D

u tT

u t T

2

n

n

T

21

nD

TT

2

( ) 2exp

( ) 1D

u t

u t T

21

2exp

1

i

i

u

u

Page 37: 2C09 Design for seismic and climate changes

Attenuation of motion

Natural logarithm of the ratio

is called logarithmic decrement

and is denoted with :

For small values of the damping

Determination of logarithmic

decrement based on peaks several

cycles apart

21

2exp

1

i

i

u

u

21

2ln

1

i

i

u

u

21 1 2

31 1 2

1 2 3 4 1

j j

j j

uuu u ue

u u u u u

1 11 ln 2jj u u

Page 38: 2C09 Design for seismic and climate changes

Free vibration tests

Determination of damping in structures: free vibration

tests

1 1ln ln

2 2

i i

i j i j

u usau

j u j u

Page 39: 2C09 Design for seismic and climate changes

References / additional reading

Anil Chopra, "Dynamics of Structures: Theory and

Applications to Earthquake Engineering", Prentice-Hall,

Upper Saddle River, New Jersey, 2001.

Clough, R.W. and Penzien, J. (2003). "Dynamics of

structures", Third edition, Computers & Structures, Inc.,

Berkeley, USA

Page 40: 2C09 Design for seismic and climate changes

[email protected]

http://steel.fsv.cvut.cz/suscos