ODE Lecture 5

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    By the term mathematical modeling, we

    mean the process whereby the behavior of areal-life system or phenomenon, whetherphysical, sociological, or even economics isdescribed by a set of Mathematical relations,after approximation and idealizations.Construction of Mathematical model startswith

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    i) Identification of the system we are

    modeling. This requires selection of somevariables as important to understanding ordescribing the behavior of the system andignoring other as marginal or irrelevant to

    this understanding.

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    ii)Making some realistic assumption, orhypothesis, about the system we aredescribing. These assumptions will alsoinclude any empirical laws that may beapplicable to the system.

    We translate these assumptions intomathematical language which usuallyresults in a set of equations and /or

    inequalities. This gives us a mathematicalmodel which will be an approximation of theactual real-life problem.

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    Once we have constructed the mathematicalmodel, we are faced with the problem ofsolving it so as to obtain the unknown variableor variables in terms of the known quantities.

    So Modeling steps are the steps thatlead from the physical situation to amathematical formulation and solution, thenphysical interpretation of the result.

    In this section we solve some model thatare described by linear first order differentialequations.

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    Let x(t) denote the population at any time t.We construct a mathematical model ofpopulation x(t) which grows or decays at a

    rate proportional tox.

    Setting up a mathematical model

    kxdt

    dx

    Growth and Decay

    Step 1

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    Step 2

    Solving the differential equation obtained.

    Step 3

    Interpretation of the result.

    kxdt

    dx

    . (1)

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    Integrating (1)

    kt

    cktxkt

    (2)

    for decay

    for growth

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    c is any arbitrary constant and can be

    determined by using initial condition andvalue of kchanges from problem to problem.

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    Example

    Bacterial Growth

    A culture initially has N0 number of bacteria.At t= 1hr the number of bacteria is measuredto be (3/2)N

    0

    . If the rate of growth is

    proportional to the number of bacteriapresent, determine the time necessary for thenumber of bacteria to triple.

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    .

    Solution

    We first solve the differential equation

    kdt

    dN. (1)

    Subject to N(0)=N0. Then we use theempirical condition to determine theconstant of proportionality k . Now eq (1) is

    both separable and linear. When it is put intothe form

    0dN

    kNdt

    ...(2)

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    We can see by inspection that the integratingfactor is . Multiplying (2) with we getkte

    ktd e Ndt

    Integrating (3)

    .(3)

    kt .. .(4)

    k te

    it follows that, at

    so equation (4) takes the form

    tcceN

    0

    0

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    kteNtN0

    .(5)

    so equation (4) takes the form

    at t= 1 , we have

    kteNN 00

    2

    3

    kte2

    3

    4055.0)2

    3ln(k

    Thus0.4055

    0( ) t

    N t N e

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    To find the time at which the bacteria havetripled we solve

    t4055.03ln

    hrt 71.24055.0

    3ln

    teNN

    4055.0

    00

    te 4055.0

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    Example

    Bacteria in a certain culture increases at a rateproportional to the number present. If thenumber of bacteria is 2000 after one hour and4000 after two hours. What was their initial

    numbers?

    Solution

    Let x be the number of bacteria at time t, then

    dxkx

    dt

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    ktcetx )(

    Solution of this equation is same as in theabove example i.e.

    . (1)

    Here we have two conditions

    (1) 2000(2) 4000

    xx

    Using these two conditions in eq (1), we get

    values of c & k.

    ln 2tx t e

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    Now we have to find the initial number when t

    = 0. x . (2)

    Equation (2) is the required initial number

    Radioactive Decay

    Radioactive decay is the process in whichan unstable atomic nucleus loses energy by

    emitting radiation in the form of particles orelectromagnetic waves

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    i) Radium is a radioactive chemical elementwhich has symbol Ra.

    ii) Radium is an alkaline earth metal. It isextremely radioactive.

    iii) Radium is used in medicines to produceradon gas which in turn is use as a cancertreatment.

    iv) Radium is over one million times moreradioactive than the same mass of Uranium.

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    Example

    Radium decomposes at a rate proportional tothe quantity of radium present. If 100 mgreduces to 90 mg in 20 years. How many milligrams will remain at the end of 1000 years?

    How long will it take for one-half of the originalamount to decompose?

    Solution

    Letx mg denote the amount of Radium presentat time t.

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    Here we the differential equation

    kxdtdx

    Solution of this equation is

    ktcetx )( (1)

    Here we have two conditions

    (0) 100

    (20) 90

    x

    x

    .....(2a)

    .(2b)

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    Appling (2a) in (1) we get

    cUsing value of c in equation (1) we get

    ktx t e ...(3)

    Appling (2b) in (1) we get2090 100 ke

    k

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    So equation (3) becomes

    t

    etx0005.0

    100)(

    Now at t = 1000 gives

    txHence after 1000 years nearly 61 mg ofradium will remain.

    t = ? Whenx = 50

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    Example

    Initially there were 100mg of a radioactivesubstance present. After 6hrs the mass decreased

    by 3%. If the rate of decay is proportional to the

    amount of the substance present at any time, find

    the amount remaining after 24 hrs?

    Solution

    Let be the initial amount, and A(t) be

    amount at any time.

    0A

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    ( ) 1 0 0A t m g(1)

    ( ) 97A t mg (2)

    at t = 0

    at t = 6

    24 , ( ) ?t hr A t

    Governing equation is

    dAkA

    dt

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    Its solution isk tA t c e

    Using condition (1) in eq (3) we get

    (3)

    c (4)

    Using the value of c in eq (3), we getktA t e

    Using condition (2) in eq (4) we get

    697 100 ke

    0.00507k

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    Using the value of k in eq (4) for t = 24 hrs,

    we get)24(00507.0100)( etA

    mgtA 5.88)(

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    Half Life

    The half life of a radioactive substance is

    the time in which half of the given amountwill disappear. Hence it measures theradioactive decay process .

    OrThe time taken for one half of a

    radioactive substance to decay is calledhalf life of the substance.

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    Example

    Determine the half-life of the radioactivesubstance described in last example.

    Solution0( )

    2

    AA t

    0.00507( )0 1002

    tAe

    Eq (1) 0.00507( )100 1002

    te

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    1ln 0 .0 0 5 0 7

    2t

    Example

    The breeder reactor converts stable uranium238 into the isotope platinum 239. After 15years it is determined that 0.043% of the initial

    amount of the platinum has disintegrated. Findthe Half Life of this isotope

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    Let A denote the amount of platinum remainingat any time t. Governing equation is

    d Ak A

    d twith

    0A A .. ..(1)

    Its solution is

    ktA t ce ..(2)

    Solution

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    Using above condition (1) in eq (2) we get

    0( ) kt

    A t A e

    0AIf 0.043% of have disintegrated, thenremaining amount is 99.957% Or 0.99957

    00.99957A A

    Now at t = 15

    Using this condition in eq (3) we get

    (3)

    15

    0 00.99957 kA A e

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    ln 0.99957

    15k

    0 . 0 0 0 0 2 8 6 7k

    0.00002867

    0( ) tA t A e

    150.99957 ke

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    24180t yrs

    1ln

    2

    0.0002867t

    1ln 0.00002867

    2t

    0.0000286700

    2

    tAA e

    0( )2

    AA t

    Now the half life in the corresponding value oftime for which

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    Carbon Dating

    About 1950, the chemist Willard deviseda method of using radio active carbon as ameans of determining the approximate ageof fossils, such as remains of woods, bones,

    etc.

    The half life of a radio active carbon isabout 5600 years. The ratio of Carbon 14 to

    ordinary Carbon in the atmosphere isconstant, and this ratio also applies toanimals and plants tissue as long as they arealive.

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    However, when the animals or plants die,

    the Carbon-14 starts to decay throughradioactivity, while the ordinary carbon doesnot disappear.

    Thus knowing the ratio of C-14 to ordinarycarbon we can determine an approximation tothe year of death.

    For his work Libby won the Nobel Prize forchemistry in 1960.

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    A wooden archeological specimen contains15% of the original Carbon-14. Using a half lifeof 5730 years. Determine the approximate ageof the specimen.

    Example

    Solution

    Governing equation is

    dA

    kAdtwith

    0)0( AA ..(1)

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    Its solution is

    ( ) k tt ce . ..(2)

    Using condition (1) in eq (2) we get.

    0( ) kt

    t A e

    5730, ( )2

    oA

    t A tat .....(3)

    Substituting condition (3) in eq (2) we get.

    57300

    02

    kA

    A e

    1ln 5730

    2k

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    k

    0( ) 0.15A t AWhen

    0.000120968

    0 0(0.15) tA A e

    ln(0.15) 0.000120968t

    15682t years