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    Chapter 10

    Dynamic response using numerical methods

    10.1 Numerical methods: introduction

    The Euler Method

    Consider the model

    constrrydt

    dy== , (10.1-1)

    From the definition of derivative,

    ttty

    dtdy

    += )(lim0

    If the time increment t is chosen small enough, the derivative

    can be replaced by the approimate epression

    t

    tytty

    dt

    dy

    +

    )()((10.1-!)

    "ssume that the right-hand side of (10.1-1) remains constantover the time interval ),( ttt + , and replace (10.1-1) by the

    follo#ing approimation$

    )()()(

    tryt

    tytty=

    +

    orttrytytty +=+ )()()( (10.1-%)

    &his techni'ue for replacing a differential e'uation #ith a

    difference e'uation is the uler method.

    'uation (10.1-%) can be #ritten in more convenient form as

    follo#s. "t the initial time ot , (10.1-%) gives

    ttrytytty ooo +=+ )()()(

    et ttt o +=1 . &hen

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    ttrytytty +=+ )()()( 111

    &hat is, (10.1-%) is applied successively at the instants kt , #herektt kk +=+1 , and #e can #rite in general

    ttrytyty kkk +=+ )()()( 1 (10.1-*)

    It is convenient to introduce a time inde k such that

    )( kk tyy

    =

    &hus, (10.1-*) becomes

    ,...!,1,0,)1(1 =+=+=+ kytrtryyky kkk (10.1-+)In this form, it is easily seen that the continuous variable )(ty

    has been represented by the discrete-time variable ky . 'uation

    (10.1-+) is a recursion relation or difference e'uation. It can be

    solved recursively (se'uentially) at the instants ,...!,1,0=k ,

    starting #ith the initial value )( oo tyy = .

    In cases #here the subscript notation is inconvenient, the

    variable ky is #ritten as )(ky . Care must be taen not to

    confuse )(ky #ith )( kty . For ,...!,1,0=k , )(ky represents )(ty at

    the values of ,...,, !1 tttt o= In this notation, (10.1-+) becomes

    ,...!,1,0),()1()1( =+=+ kkytrky (10.1-)ith ra constant, #e can easily solve the original differential

    e'uation (10.1-1), so #e really have no need for (10.1-).

    /o#ever, this is not the case for a general e'uation of the form

    ),( vyfy =

    (10.1-)

    "ssume the right-hand side to be constant over the interval),( 1+kk tt and e'ual to the value )(),(2 kk tvtyf . ith the

    approimation (10.1-!), #e have the uler method for (10.1-).

    )(),(2)()( 1 kkkk tvtytftyty +=+ (10.1-3)

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    &his is easily programmed on a computer. &he values of,),(, ttyt

    oo and any parameters in the functions f and v must

    be read into the program along #ith a stopping criterion.

    &he uler method is the simplest algorithm for numerical

    solution of a differential e'uation, but it usually gives the least

    accurate results.

    Example 10.1

    Compare the eact solution and the uler method using a step

    si4e 1.0=t for

    1)0(, ==

    ytyy #here 10 t

    &he uler algorithm (10.1-3) for this model is

    )()1.01()( 1 kkk tytty +=+ (10.1-5)

    For this case, the eact solution can be obtained by separating

    variables and direct integration. First #e #rite

    tdty

    dy =

    and integrate to obtain

    =tty

    y

    tdty

    dy

    0

    )(

    )0(

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    or

    !ln

    !)(

    )0(

    ty

    ty

    y =

    &his can be rearranged as

    )!6ep()0()( !tyty =

    &he follo#ing table compares the results.kt )( kty

    act uler

    0.1 1.00+ 1.0000.! 1.0!0 1.010

    0.5 1.*55 1.*15

    1.0 1.*5 1.+*

    &he error in the uler method increases #ith time. It is in error

    by 0.+7 in the first step8 by the tenth step, the error is .157.

    &he accuracy can be improved by using a smaller value of t

    .

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    Selecting a step size

    &hus far, #e have not considered the effect of the 9run time9 of

    a numerical method. &his is the time re'uired for the soft#are to

    perform the calculations, and it is fre'uently an important factor

    in selecting an algorithm. It is difficult to mae a prior

    determination of the run time for a given algorithm.

    &he process of selecting a proper si4e t begins by considering

    the dynamics of the model and ho# fast the input changes #ith

    time. " trial value of t is then selected that is small in relation

    to these considerations. &he trial solution for the response is

    obtained #ith this value. &he step si4e is then reduced

    significantly, and the responses are compared. If they agree tothe number of significant figures specified by the analyst, the

    correct ans#er is taen to be the last solution. If not, t is again

    reduced by a significant factor and the process is repeated until

    the solution converges.

    In strictly analytical terms, as t approaches 4ero, the solution

    of the difference e'uation approaches that of the corresponding

    differential e'uation. &his is the reason for using a small t .

    &he error produced #hen t is not small enough to representthe differential e'uation accurately is termed truncation error.

    /o#ever, numerical considerations as #ell as computer time

    re'uire not maing t too small. &he reason is that the effect of

    round-off error is greater for smaller t due to the larger

    number of iterations re'uired.

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    10.2 Advanced numerical methods

    In light of the large variety of e'uation types that are nonlinear,

    it is no #onder that many different numerical methods eist for

    solving them. /ere, #e consider t#o methods that are generally

    useful. &he first is a so-called predictor-corrector method based

    on the uler method but #ith greater accuracy. &he second

    method is the :unge-;utta family of algorithms.

    Trapezoidal integration

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    &he difference bet#een the uler and trape4oidal integration

    methods is sho#n in Figure 10.1. &he shaded area represents the

    approimation to the integral

    +1

    )(k

    k

    t

    t

    dv

    =oth methods use a rectangle of #idth t . &he uler method

    taes the height of the rectangle to be )( ktv and approimates

    the integral as$

    +

    =

    1

    )()(

    k

    k

    t

    t

    kttvdv

    >n the other hand, the trape4oidal method taes the rectangle?s

    height as the average value @v of )( ktv and )( 1+ktv andapproimates the integral #ith (10.!-%)

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    Figure 10.1 Comparison of the uler and trape4oidal integration

    approimations. &he shaded area represents the approimation

    to the integral. (a) uler. (b) &rape4oidal.

    redictor!corrector methods

    "s can be seen from Figure 10.1, the uler method can haveserious deficiency in problems, #here the variables are rapidly

    changing, because the method assumes the variables are

    constant over the time interval t . "s a result, its truncation

    error can be sho#n to be the order of !)( t .

    >ne #ay of improving the method #ould be by using a better

    approimation to the right-hand side of the model

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    ),,( tvyfdt

    dy= (10.!-+)

    #here v is the input function. &he uler approimation is

    [ ]kkkkk ttvtyfttyty ),(),()()( 1 +=+ (10.!-)

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    Euler predictor:

    ),,(1 kkkkk tvyftyx +=+ (10.!-5)

    Trapezoidal corrector:

    [ ]),,(),,(!

    1111 ++++ +

    += kkkkkkkk tvxftvyft

    yy (10.!-10)

    &his algorithm is sometimes called the modified uler method.

    /o#ever, note that any algorithm can be tried as a predictor or a

    corrector. &hus many methods can be classified as predictor-corrector, but #e #ill limit our treatment to the modified uler

    method. &he truncation error for this method is of the order of%)( t , a significant improvement over the !)( t error of the

    basic uler method.

    For purposes of comparison #ith the :unge-;utta methods to

    follo#, #e can epress the modified uler method as$

    ),,(1 kkk tvyftg = (10.!-11)

    ),,( 11! ttvgyftg kkk ++= + (10.!-1!)

    )(!

    1!11

    ggyykk ++=+ (10.!-1%)

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    Example 10.2

    Ase the modified uler method #ith 1.0=t to solve the

    e'uation 1)0(, == ytydt

    dyup to time 0.1=t .

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    replace 1+kx on the right-hand side of that e'uation in order to

    get an improved estimate of 1+ky . &his is repeated until the

    desired accuracy is achieved8 then the net t interval is treated

    the same #ay. /o#ever, this modification obviously increases

    the compleity of the programming.

    "unge!#utta methods

    &he &aylor series representation forms the basis of several

    methods for solving differential e'uations, including the :unge-

    ;utta methods. &he &aylor series may be used to represent the

    solution )( tty + in terms of )(ty and its derivatives as follo#s.

    ...)()(-

    1)()(

    !

    1)()()( %! ++++=+

    tyttyttyttytty (10.!-1*)

    &he re'uired derivatives are calculated from the differential

    e'uation. For an e'uation of the form

    ),( ytfdtdy = (10.!-1+)

    these derivatives are

    ),()( ytfty =

    dt

    dfty =

    )(

    etc.,)(!

    !

    dt

    fdty =

    (10.!-1)

    #here (10.!-1+) is to be used to epress the derivatives in terms

    of only )(ty . If these derivatives can be found, (10.!-1*) can be

    used to march for#ard in time. In practice, the high order

    derivatives can be difficult to calculate, and the series (10.!-1*)

    is truncated at some term. &he number of terms ept in the

    series thus determines its accuracy. If terms up to and including

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    nthderivative of y are retained, the truncation error at each step

    is of the order of the first term dropped-namely,

    1

    11

    )C1(

    )(

    +

    ++

    +

    n

    nn

    dt

    yd

    n

    t

    (10.!-1)

    sometimes the closed-form epression for the series can be

    recogni4ed. For eample, consider the e'uation

    0,!

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    )(1

    )()(

    tyta

    tytty

    =+ (10.!-15)

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    1!1 =+ww (10.!-!+)

    !

    11 =w

    (10.!-!)

    !

    1! =w (10.!-!)

    &hus, the family of second-order :unge-;utta algorithms is

    categori4ed by the parameters ),,,( !1 ww , one of #hich can be

    chosen independently. &he choice%

    != minimi4es the

    truncation error term. For 1= , the :unge-;utta algorithm(10.!-!1)-(10.!-!%) corresponds to the trape4oidal integration

    rule if f is a function of only t , and is the same as the

    predictor-corrector algorithm (10.!-5)-(10.!-10) for a general),( tyf .

    %ourth!order algorithms

    &he algorithm is

    **%%!!111 gwgwgwgwyy kk ++++=+ (10.!-!3)

    )(,2

    )(,2

    ),(

    ),(

    1%%%%%!%%*

    1!!!!!%

    111!

    1

    gggyhthfg

    ggyhthfg

    gyhthfg

    ythfg

    kk

    kk

    kk

    kk

    ++++=

    +++=

    ++=

    =

    (10.!-!5)

    Comparison #ith the &aylor series yields eight e'uations for the

    ten parameters. &hus, t#o parameters can be chosen in light of

    other considerations. &hree common choices are as follo#s.

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    1.Gill's method. &his choice minimi4es the number of memory

    locations re'uired to implement the algorithm and thus is #ell

    suited for programmable calculators.

    !611

    !618!611

    18!61

    8%6)!611(8%6)!611(8-61

    %

    %!

    %!1

    %!*1

    +=

    ==

    ===

    +====

    wwww

    (10.!-%0)

    2.Ralston's method. &his choice minimi4es a bound on the

    truncation error.

    0+05-+1-.%81+3+5-*.083%!3-*-.%

    18*++%!+.08*.0

    1113*3.08!0++%+-0.18++1*30--.081*-0!3.0

    %!%

    %!1

    *%!1

    ===

    ===

    ====

    wwww

    (10.!-%1)

    &.lassical method. &his method reduces to

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    Example 10.3

    Ase the classical :unge-;utta parameter values (10.!-%!) #ith a

    step si4e 1.0== th to solve

    1.0toup1)0(, ===

    tytyy

    &he algorithm for the classical parameter value is

    )101(0,2

    )!

    1

    !

    1(

    !

    1,

    !

    12

    )!

    1,

    !

    1(

    ),(

    -

    1

    %

    1

    %

    1

    -

    1

    1%!*

    1!%

    1!

    1

    *%!11

    gggyhthfg

    ggyhthfg

    gyhthfg

    ythfg

    ggggyy

    kk

    kk

    kk

    kk

    kk

    ++++=

    +++=

    ++=

    =

    ++++=+

    For the given problem, tyf = . For the first iteration,1,0,0 00 === ytk

    and

    0100+01!+.0)00+01!+.01)(1.00(1.0

    00+01!+.0)00+.0!

    11)(0+.00(1.0

    00+.0)0!

    1

    1)(0+.00(1.0

    0)0(1.0

    *

    %

    !

    1

    =++=

    =++=

    =++=

    ==

    g

    g

    g

    g

    &hus,

    00+01!+!1.1)0100+01!+.0(-

    1)00+01!+.0(

    %

    1)00+.0(

    %

    10

    -

    11)1.0(

    1 =++++== yy

    &his ans#er agrees #ith the eact solution )!6ep( !t . &he rest of

    the solution is as follo#s.t 0.1 0.! 0.5 1.0

    )(ky 1.00+01!+!1 1.0!0!01%* 1.*55%0!%! 1.*3!100

    &he eact solution at 0.1=t , to ten figures, is 1.*3!1!1. &he

    numerical solution is correct to seven figures.

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    10.& Conversion to state varia'le $orm

    &here are several #ays of converting a model to state variable

    form. If the variables representing the energy storage in the

    system are chosen as the state variables, the model must then be

    manipulated algebraically to produce the standard state variable

    form. &he re'uired algebra is not al#ays obvious. /o#ever, #e

    note here that the model

    =

    )(,,...,,1

    1

    tvdt

    yd

    dt

    dyytf

    dt

    ydn

    n

    n

    n

    (10.%-1)

    #ith the input )(tv can al#ays put into state variable form by

    the follo#ing choice of state variables$

    1

    1

    !

    1

    =

    =

    =

    n

    n

    ndt

    ydx

    dt

    dyx

    yx

    (10.%-!)

    &he resulting state model is$

    [ ])(,,...,,, !1

    1

    %!

    !1

    tvxxxtfx

    xx

    xx

    xx

    nn

    nn

    =

    =

    =

    =

    (10.%-%)

    &he numbering scheme is not uni'ue8 in fact, #e often find thefollo#ing state variable choice$

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    yy

    dt

    dyy

    dt

    ydy

    dt

    ydy

    n

    n

    n

    n

    n

    n

    =

    =

    =

    =

    1

    !

    !

    !

    1

    1

    1

    (10.%-*)

    #hich gives the model

    [ ]

    1

    !%

    1!

    111 )(,,...,,,

    =

    =

    =

    =

    nn

    nn

    yy

    yy

    yy

    tvyyytfy

    (10.%-+)

    Coupled higher order models

    'uation (10.%-1) is some#hat general in that it can be

    nonlinear, but it does not cover all cases. For eample, considerthe coupled higher order model

    ),,,,(1

    = zzyytfy (10.%-)

    ),,,,(!

    = zzyytfz (10.%-)

    Choose the state variables as$

    =

    =

    =

    =

    zx

    zx

    yx

    yx

    *

    %

    !

    1

    (10.%-3)

    &hen the state model is$

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    ),,,,(

    ),,,,(

    *%!1!*

    *%

    *%!11!

    !1

    xxxxtfx

    xx

    xxxxtfx

    xx

    =

    =

    =

    =

    (10.%-5)

    State e(uations $rom trans$er $unctions

    e no# illustrate a method for using the transfer function to

    rearrange the diagram so that state variables can be identified.

    &he order of the system, and therefore the number of state

    variables re'uired, can be found by eamining the denominator

    of the transfer functions. If the denominator polynomial is oforder n, then nstate variables are re'uired. Dhysical

    considerations (integral causality) can be used to sho# that the

    outputs of integration processes )61( s can be chosen as state

    variables.

    &o illustrate ho# a state model can be derived from a transfer

    function, consider the follo#ing first-order model #ith

    numerator dynamics$

    1

    10

    )(

    )()(

    as

    !s!

    s"

    s#sT

    +

    +== (10.%-10)

    #here the input is u and the output is y . Cross-multiplying and

    reverting to the time domain, #e obtain

    u!u!yay 101 +=+

    (10.%-11)

    "n alternative #ay of obtaining the differential e'uation is by

    dividing the numerator and denominator of (10.%-10) by s .

    )(

    )(

    61

    6)(

    1

    10

    s"

    s#

    sa

    s!!sT =

    +

    += (10.%-1!)

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    &he essence of the techni'ue is to obtain a 919 in the

    denominator, #hich is then used to isolate )(s# . Cross-

    multiplying gives

    [ ] )()()(1

    )()()()( 0111

    01 s"!s#as"!

    ss"

    s

    !s"!s#

    s

    as# +=++=

    &he term multiplying s61 is the input to an integrator8 the

    integrator?s output can be selected as a state variable x . &hus,

    [ ] [ ])()()(1)()(1)(

    )()()(

    011111

    0

    s"!as$as"!s

    s#as"!s

    s$

    s"!s$s#

    ==

    +=

    or

    u!a!xax )( 0111 +=

    (10.%-1%)

    u!xy0

    += (10.%-1*)

    &he bloc diagram is sho#n in Figure 10.!. Compare (10.%-11)

    #ith (10.%-1%), and note that the derivative of the input does not

    appear in the latter form.

    Figure 10.! &he bloc diagram for (10.%-1%) and (10.%-1*).

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    Eo#, consider the second-order model for the mechanical

    vibration problem. Its transfer function is$

    kcsmss%

    s$sT

    ++==

    !

    1

    )(

    )()( (10.%-1+)

    ivide by !ms to obtain a unity term.

    !

    !

    661

    61

    )(

    )()(

    mskmsc

    ms

    s%

    s$sT

    ++==

    Cross-multiply and rearrange to identify the integration

    operators.

    +=

    +=

    )()(11

    )(1

    )(1

    )()()(!!

    s$m

    ks%

    mss$

    m

    c

    s

    s%ms

    s$ms

    ks$

    ms

    cs$

    (10.%-1)

    efining the state variables as the outputs of the integrators, #esee that

    =

    +==

    )()(11

    )(

    )()(1

    )()(

    !

    !1

    s$m

    ks%

    mss$

    s$s$m

    c

    ss$s$

    or

    =

    +=

    )()(11

    )(

    )()(1

    )(

    1!

    !11

    s$m

    ks%

    mss$

    s$s$m

    c

    ss$

    Figure 10.%a is the bloc diagram derived from these relations.

    183

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    Figure 10.% &he bloc diagram for the vibration model (10.%-

    1+). (a) iagram for the state model (10.%-1) and (10.%-13). (b)

    iagram for the state model (10.%-15) and (10.%-!0).

    &he corresponding state e'uations in standard form are$

    !11 xxm

    cx +=

    (10.%-1)

    fm

    xm

    kx

    11!

    +=

    (10.%-13)

    #here xx =1 .

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    'uation (10.%-1) can also be arranged as follo#s. et

    )()(

    )()(

    1!

    1

    ss$s$

    sm$s$

    =

    =

    &hen

    = )()()(

    1)( 1!! s$

    m

    ks$

    m

    cs%

    ss$

    &hese relations give the diagram sho#n in Figure 10.%b. &he

    resulting state model #ith mxx =1 is

    !1 xx =

    (10.%-15)

    fxm

    cx

    m

    kx +=

    !1! (10.%-!0)

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    State varia'le models and numerator dynamics

    &he general time-invariant model #ith numerator dynamics can

    be #ritten as$

    01

    1

    1

    01

    1

    1

    ...

    ...

    )(

    )(

    asasasa

    !s!s!s!

    s&

    s#

    n

    n

    n

    n

    n

    n

    n

    n

    ++++

    ++++=

    (10.%-!1)

    ividing the numerator and denominator byn

    nsa gives

    nnn

    nn

    nn

    sss

    sss

    s&

    s#

    ++++

    ++++=

    01

    11

    1

    0

    1

    1

    1

    1

    ...1

    ...

    )(

    )(

    (10.%-!!)

    #here nii a! 6= and nii aa 6= . &his gives

    { }...)()(2)()()( !!1

    11

    1

    00

    !

    !!

    1

    11

    +++=

    ++

    +

    +=

    s#s&ss#s&ss&

    #'s()s&'s(*+,-......

    #'s()s&'s( *+, -

    #'s()s+&'s(,-&'s(-#'s(

    nnnnn

    *n

    *

    n*n*

    nnn

    e choose the output of each integrator )61( s to be a state

    variable. &hus,

    )()(2)(

    .

    .

    .

    )()()(2)(

    )()()(2)(

    )()()(

    00

    1

    %!!

    1

    !

    !11

    1

    1

    1

    s#s&ss$

    s$s#s&ss$

    s$s#s&ss$

    s$s&s#

    n

    nn

    nn

    n

    =

    +=

    +=

    +=

    (10.%-!%)

    Ase the first e'uation in (10.%-!%) to eliminate G(s) in the

    remaining e'uations. &hus,

    )()()()(.

    .

    )()()()()(

    )()()()()(

    1000

    %1!!!!

    !11111

    s$s&ss$

    s$s$s&ss$

    s$s$s&ss$

    nn

    nnnn

    nnnn

    =

    +=

    +=

    186

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    &his gives the differential e'uation set

    100

    %1!!

    !111

    !

    1

    xvx

    xxvx

    xxvx

    n

    n

    n

    n

    n

    =

    +=

    +=

    (10.%-!*)

    #here

    niii =

    (10.%-!+)

    1xvy

    n += (10.%-!)

    &he original initial conditions of the problem are given in terms

    of y , as .),0(),0(),0( etcyyy

    'uations (10.%-!*) and (10.%-!) can

    be used to find the relation bet#een )0(ix and ),...0(),0(),(

    yytv

    From (10.%-!), at 0=t $

    )0()0()0(1 vyx n= (10.%-!)

    "lso, from the first e'uation in (10.%-!*), #e have

    vxxx nn 1111!

    += (10.%-!3)

    187

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    ifferentiating (10.%-!) and substituting gives

    vvvyy

    vvyvy

    vxvyx

    nnnn

    nnnnn

    nnn

    111

    111

    111!

    )(

    ++=

    +=

    +=

    Henerali4ing this procedure and denoting ii dtyd 6 by )(iy gives

    the result$

    vvvv

    yyyx

    inin

    i

    n

    i

    n

    in

    i

    n

    i

    i

    11

    )!(

    1

    )1(

    1

    )!(

    1

    )1(

    ...2

    ...

    ++

    +

    +++

    +++=

    (10.%-!5)

    #here ni ,...,!,1=

    &hus the initial values )0(ix can be found from (10.%-!5) given

    the initial values of ),(),( tvty and their derivatives. Interpreting0=t as e'uivalent to = 0t , #e can tae 0...)0()0( ===

    vv . In this

    case (10.%-!5) gives

    )0(...)0()0()0( 1)!(

    1

    )1(

    yyyx ini

    n

    i

    i +

    +++= (10.%-%0)

    &he transformation to state variable form is summari4ed in

    &able 10.1

    188

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    &able 10.1 " state variable form for numerator dynamics

    For eample, consider

    -+10

    !%

    )(

    )(!

    !

    ++

    ++=

    ss

    ss

    s&

    s#(10.%-%1)

    #here 0for0)(and,)0(,*)0( ===

    ttvyy . &he state model (10.%-

    !*) and (10.%-!) is$

    !11 +.0!+.0 xxvx +=

    (10.%-%!)

    1! -.01*.0 xvx =

    (10.%-%%)

    11.0 xvy += (10.%-%*)

    &he initial conditions are, from (10.%-%0),

    *)0()0(1 == yx (10.%-%+)

    189

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    5!)0(+.0)0()0(! =+=+=

    yyx (10.%-%)

    'uations (10.%-%!)-(10.%-%*) are interpreted for 0>t . &hus,

    from (10.%-%*)-(10.%-%+), #e see that*)0(1.0)0( ++=+ vy

    . If)(tv

    is a unit step, then 1)0( =+v and 1.*)0( =+y .