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Sec on 3.4
    Exponen al Growth and Decay
            V63.0121.011: Calculus I
          Professor Ma hew Leingang
                 New York University


               March 23, 2011


.
Announcements


   Quiz 3 next week in
   recita on on 2.6, 2.8, 3.1,
   3.2
Objectives

   Solve the ordinary
   differen al equa on
   y′ (t) = ky(t), y(0) = y0
   Solve problems involving
   exponen al growth and
   decay
Outline
 Recall
 The differen al equa on y′ = ky
 Modeling simple popula on growth
 Modeling radioac ve decay
   Carbon-14 Da ng
 Newton’s Law of Cooling
 Con nuously Compounded Interest
Derivatives of exponential and
logarithmic functions
               y          y′

              ex          ex

              ax      (ln a) · ax
                          1
              ln x
                          x
                        1 1
             loga x        ·
                       ln a x
Outline
 Recall
 The differen al equa on y′ = ky
 Modeling simple popula on growth
 Modeling radioac ve decay
   Carbon-14 Da ng
 Newton’s Law of Cooling
 Con nuously Compounded Interest
What is a differential equation?
 Defini on
 A differen al equa on is an equa on for an unknown func on
 which includes the func on and its deriva ves.
What is a differential equation?
 Defini on
 A differen al equa on is an equa on for an unknown func on
 which includes the func on and its deriva ves.
 Example

     Newton’s Second Law F = ma is a differen al equa on, where
     a(t) = x′′ (t).
What is a differential equation?
 Defini on
 A differen al equa on is an equa on for an unknown func on
 which includes the func on and its deriva ves.
 Example

     Newton’s Second Law F = ma is a differen al equa on, where
     a(t) = x′′ (t).
     In a spring, F(x) = −kx, where x is displacement from
     equilibrium and k is a constant. So
                                               k
              −kx(t) = mx′′ (t) =⇒ x′′ (t) +     x(t) = 0.
                                               m
Showing a function is a solution
 Example (Con nued)
 Show that x(t) = A sin ωt + B cos ωt sa sfies the differen al
                k                   √
 equa on x′′ + x = 0, where ω = k/m.
               m
Showing a function is a solution
 Example (Con nued)
 Show that x(t) = A sin ωt + B cos ωt sa sfies the differen al
                k                   √
 equa on x′′ + x = 0, where ω = k/m.
               m
 Solu on
 We have

                   x(t) = A sin ωt + B cos ωt
                  x′ (t) = Aω cos ωt − Bω sin ωt
                  x′′ (t) = −Aω 2 sin ωt − Bω 2 cos ωt
The Equation y′ = 2
 Example

    Find a solu on to y′ (t) = 2.
    Find the most general solu on to y′ (t) = 2.
The Equation y′ = 2
 Example

    Find a solu on to y′ (t) = 2.
    Find the most general solu on to y′ (t) = 2.

 Solu on
    A solu on is y(t) = 2t.
The Equation y′ = 2
 Example

    Find a solu on to y′ (t) = 2.
    Find the most general solu on to y′ (t) = 2.

 Solu on
    A solu on is y(t) = 2t.
    The general solu on is y = 2t + C.
The Equation y′ = 2
 Example

      Find a solu on to y′ (t) = 2.
      Find the most general solu on to y′ (t) = 2.

 Solu on
      A solu on is y(t) = 2t.
      The general solu on is y = 2t + C.

 Remark
 If a func on has a constant rate of growth, it’s linear.
The Equation y′ = 2t
 Example

    Find a solu on to y′ (t) = 2t.
    Find the most general solu on to y′ (t) = 2t.
The Equation y′ = 2t
 Example

    Find a solu on to y′ (t) = 2t.
    Find the most general solu on to y′ (t) = 2t.

 Solu on
    A solu on is y(t) = t2 .
The Equation y′ = 2t
 Example

    Find a solu on to y′ (t) = 2t.
    Find the most general solu on to y′ (t) = 2t.

 Solu on
    A solu on is y(t) = t2 .
    The general solu on is y = t2 + C.
The Equation y′ = y
 Example

    Find a solu on to y′ (t) = y(t).
    Find the most general solu on to y′ (t) = y(t).
The Equation y′ = y
 Example

    Find a solu on to y′ (t) = y(t).
    Find the most general solu on to y′ (t) = y(t).

 Solu on
    A solu on is y(t) = et .
The Equation y′ = y
 Example

      Find a solu on to y′ (t) = y(t).
      Find the most general solu on to y′ (t) = y(t).

 Solu on
      A solu on is y(t) = et .
      The general solu on is y = Cet , not y = et + C.
 (check this)
Kick it up a notch: y′ = 2y
 Example

    Find a solu on to y′ = 2y.
    Find the general solu on to y′ = 2y.
Kick it up a notch: y′ = 2y
 Example

    Find a solu on to y′ = 2y.
    Find the general solu on to y′ = 2y.

 Solu on
    y = e2t
    y = Ce2t
In general: y′ = ky
 Example

    Find a solu on to y′ = ky.
    Find the general solu on to y′ = ky.
In general: y′ = ky
 Example

     Find a solu on to y′ = ky.
     Find the general solu on to y′ = ky.

 Solu on
    y = ekt
    y = Cekt
In general: y′ = ky
 Example

     Find a solu on to y′ = ky.
     Find the general solu on to y′ = ky.

 Solu on                            Remark
    y = ekt                         What is C? Plug in t = 0:
    y = Cekt                           y(0) = Cek·0 = C · 1 = C,

                                    so y(0) = y0 , the ini al value
                                    of y.
Constant Relative Growth =⇒
Exponential Growth
 Theorem
 A func on with constant rela ve growth rate k is an exponen al
 func on with parameter k. Explicitly, the solu on to the equa on

                     y′ (t) = ky(t)    y(0) = y0

 is
                             y(t) = y0 ekt
Exponential Growth is everywhere
   Lots of situa ons have growth rates propor onal to the current
   value
   This is the same as saying the rela ve growth rate is constant.
   Examples: Natural popula on growth, compounded interest,
   social networks
Outline
 Recall
 The differen al equa on y′ = ky
 Modeling simple popula on growth
 Modeling radioac ve decay
   Carbon-14 Da ng
 Newton’s Law of Cooling
 Con nuously Compounded Interest
Bacteria
   Since you need bacteria
   to make bacteria, the
   amount of new bacteria
   at any moment is
   propor onal to the total
   amount of bacteria.
   This means bacteria
   popula ons grow
   exponen ally.
Bacteria Example
 Example
 A colony of bacteria is grown under ideal condi ons in a laboratory.
 At the end of 3 hours there are 10,000 bacteria. At the end of 5
 hours there are 40,000. How many bacteria were present ini ally?
Bacteria Example
 Example
 A colony of bacteria is grown under ideal condi ons in a laboratory.
 At the end of 3 hours there are 10,000 bacteria. At the end of 5
 hours there are 40,000. How many bacteria were present ini ally?

 Solu on
 Since y′ = ky for bacteria, we have y = y0 ekt . We have

             10, 000 = y0 ek·3            40, 000 = y0 ek·5
Bacteria Example Solution
 Solu on (Con nued)
 We have

             10, 000 = y0 ek·3             40, 000 = y0 ek·5

 Dividing the first into the second gives

       40, 000 y0 e5k
              =     3k
                       =⇒ 4 = e2k =⇒ ln 4 = ln(e2k ) = 2k
       10, 000 y0 e
                ln 4 ln 22   2 ln 2
        =⇒ k =       =     =        = ln 2
                 2      2       2
Solu on (Con nued)
Since y = y0 et ln 2 , at me t = 3 we have
                                               10, 000
       10, 000 = y0 e3 ln 2 = y0 · 8 =⇒ y0 =           = 1250
                                                  8
Outline
 Recall
 The differen al equa on y′ = ky
 Modeling simple popula on growth
 Modeling radioac ve decay
   Carbon-14 Da ng
 Newton’s Law of Cooling
 Con nuously Compounded Interest
Modeling radioactive decay
 Radioac ve decay occurs because many large atoms spontaneously
 give off par cles.
Modeling radioactive decay
 Radioac ve decay occurs because many large atoms spontaneously
 give off par cles.
 This means that in a sample of a
 bunch of atoms, we can assume a
 certain percentage of them will “go
 off” at any point. (For instance, if all
 atom of a certain radioac ve element
 have a 20% chance of decaying at any
 point, then we can expect in a
 sample of 100 that 20 of them will be
 decaying.)
Radioactive decay as a differential equation
  The rela ve rate of decay is constant:
                                 y′
                                    =k
                                 y
  where k is nega ve.
Radioactive decay as a differential equation
  The rela ve rate of decay is constant:
                                 y′
                                    =k
                                 y
  where k is nega ve. So

                        y′ = ky =⇒ y = y0 ekt

  again!
Radioactive decay as a differential equation
  The rela ve rate of decay is constant:
                                 y′
                                    =k
                                 y
  where k is nega ve. So

                        y′ = ky =⇒ y = y0 ekt

  again!
  It’s customary to express the rela ve rate of decay in the units of
  half-life: the amount of me it takes a pure sample to decay to one
  which is only half pure.
Computing the amount remaining
 Example
 The half-life of polonium-210 is about 138 days. How much of a
 100 g sample remains a er t years?
Computing the amount remaining
 Example
 The half-life of polonium-210 is about 138 days. How much of a
 100 g sample remains a er t years?

 Solu on
 We have y = y0 ekt , where y0 = y(0) = 100 grams. Then
                                                    365 · ln 2
              50 = 100ek·138/365 =⇒ k = −                      .
                                                      138
 Therefore
                y(t) = 100e−              = 100 · 2−365t/138
                               365·ln 2
                                 138 t
Computing the amount remaining
 Example
 The half-life of polonium-210 is about 138 days. How much of a
 100 g sample remains a er t years?

 Solu on
 We have y = y0 ekt , where y0 = y(0) = 100 grams. Then
                                                    365 · ln 2
              50 = 100ek·138/365 =⇒ k = −                      .
                                                      138
 Therefore
                y(t) = 100e−              = 100 · 2−365t/138
                               365·ln 2
                                 138 t
Carbon-14 Dating
             The ra o of carbon-14 to carbon-12 in
             an organism decays exponen ally:

                           p(t) = p0 e−kt .

             The half-life of carbon-14 is about 5700
             years. So the equa on for p(t) is

                   p(t) = p0 e− 5700 t = p0 2−t/5700
                                 ln2
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?

 Solu on
                                               p(t)
 We are looking for the value of t for which        = 0.1.
                                                p0
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?

 Solu on
                                               p(t)
 We are looking for the value of t for which        = 0.1. From the equa on we have
                                                p0

    2−t/5700 = 0.1
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?

 Solu on
                                               p(t)
 We are looking for the value of t for which        = 0.1. From the equa on we have
                                                p0
                              t
    2−t/5700 = 0.1 =⇒ −          ln 2 = ln 0.1
                            5700
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?

 Solu on
                                               p(t)
 We are looking for the value of t for which        = 0.1. From the equa on we have
                                                p0
                              t                       ln 0.1
    2−t/5700 = 0.1 =⇒ −          ln 2 = ln 0.1 =⇒ t =        · 5700
                            5700                       ln 2
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?

 Solu on
                                               p(t)
 We are looking for the value of t for which        = 0.1. From the equa on we have
                                                p0
                              t                       ln 0.1
    2−t/5700 = 0.1 =⇒ −          ln 2 = ln 0.1 =⇒ t =        · 5700 ≈ 18, 940
                            5700                       ln 2
Computing age with Carbon-14
 Example
 Suppose a fossil is found where the ra o of carbon-14 to carbon-12
 is 10% of that in a living organism. How old is the fossil?

 Solu on
                                               p(t)
 We are looking for the value of t for which        = 0.1. From the equa on we have
                                                p0
                              t                       ln 0.1
    2−t/5700 = 0.1 =⇒ −          ln 2 = ln 0.1 =⇒ t =        · 5700 ≈ 18, 940
                            5700                       ln 2
 So the fossil is almost 19,000 years old.
Outline
 Recall
 The differen al equa on y′ = ky
 Modeling simple popula on growth
 Modeling radioac ve decay
   Carbon-14 Da ng
 Newton’s Law of Cooling
 Con nuously Compounded Interest
Newton’s Law of Cooling
   Newton’s Law of Cooling states
   that the rate of cooling of an
   object is propor onal to the
   temperature difference between
   the object and its surroundings.
Newton’s Law of Cooling
   Newton’s Law of Cooling states
   that the rate of cooling of an
   object is propor onal to the
   temperature difference between
   the object and its surroundings.
   This gives us a differen al
   equa on of the form
           dT
              = k(T − Ts )
           dt
   (where k < 0 again).
General Solution to NLC problems
                           ′ ′
 To solve this, change the variable y(t) = T(t) − Ts . Then y = T and
 k(T − Ts ) = ky. The equa on now looks like
                     dT                     dy
                        = k(T − Ts ) ⇐⇒        = ky
                     dt                     dt
General Solution to NLC problems
                           ′ ′
 To solve this, change the variable y(t) = T(t) − Ts . Then y = T and
 k(T − Ts ) = ky. The equa on now looks like
                     dT                     dy
                        = k(T − Ts ) ⇐⇒        = ky
                     dt                     dt
 Now we can solve!
    y′ = ky
General Solution to NLC problems
                           ′ ′
 To solve this, change the variable y(t) = T(t) − Ts . Then y = T and
 k(T − Ts ) = ky. The equa on now looks like
                     dT                     dy
                        = k(T − Ts ) ⇐⇒        = ky
                     dt                     dt
 Now we can solve!
    y′ = ky =⇒ y = Cekt
General Solution to NLC problems
                           ′ ′
 To solve this, change the variable y(t) = T(t) − Ts . Then y = T and
 k(T − Ts ) = ky. The equa on now looks like
                     dT                     dy
                        = k(T − Ts ) ⇐⇒        = ky
                     dt                     dt
 Now we can solve!
    y′ = ky =⇒ y = Cekt =⇒ T − Ts = Cekt
General Solution to NLC problems
                           ′ ′
 To solve this, change the variable y(t) = T(t) − Ts . Then y = T and
 k(T − Ts ) = ky. The equa on now looks like
                     dT                     dy
                        = k(T − Ts ) ⇐⇒        = ky
                     dt                     dt
 Now we can solve!
    y′ = ky =⇒ y = Cekt =⇒ T − Ts = Cekt =⇒ T = Cekt + Ts
General Solution to NLC problems
                           ′ ′
 To solve this, change the variable y(t) = T(t) − Ts . Then y = T and
 k(T − Ts ) = ky. The equa on now looks like
                     dT                     dy
                        = k(T − Ts ) ⇐⇒        = ky
                     dt                     dt
 Now we can solve!
    y′ = ky =⇒ y = Cekt =⇒ T − Ts = Cekt =⇒ T = Cekt + Ts
 Plugging in t = 0, we see C = y0 = T0 − Ts . So
 Theorem
 The solu on to the equa on T′ (t) = k(T(t) − Ts ), T(0) = T0 is

                       T(t) = (T0 − Ts )ekt + Ts
Computing cooling time with NLC
 Example
 A hard-boiled egg at 98 ◦ C is put in a sink of 18 ◦ C water. A er 5
 minutes, the egg’s temperature is 38 ◦ C. Assuming the water has
 not warmed appreciably, how much longer will it take the egg to
 reach 20 ◦ C?
Computing cooling time with NLC
 Example
 A hard-boiled egg at 98 ◦ C is put in a sink of 18 ◦ C water. A er 5
 minutes, the egg’s temperature is 38 ◦ C. Assuming the water has
 not warmed appreciably, how much longer will it take the egg to
 reach 20 ◦ C?
 Solu on
 We know that the temperature func on takes the form

                 T(t) = (T0 − Ts )ekt + Ts = 80ekt + 18

 To find k, plug in t = 5 and solve for k.
Finding k
 Solu on (Con nued)

         38 = T(5) = 80e5k + 18
Finding k
 Solu on (Con nued)

         38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k
Finding k
 Solu on (Con nued)

         38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k
          1
            = e5k
          4
Finding k
 Solu on (Con nued)

         38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k
                         ( )
          1                1
            = e5k =⇒ ln       = 5k
          4                4
Finding k
 Solu on (Con nued)

         38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k
                         ( )
          1                1                 1
            = e5k =⇒ ln       = 5k =⇒ k = − ln 4.
          4                4                 5
Finding k
 Solu on (Con nued)

           38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k
                           ( )
            1                1                 1
              = e5k =⇒ ln       = 5k =⇒ k = − ln 4.
            4                4                 5
 Now we need to solve for t:

                     20 = T(t) = 80e− 5 ln 4 + 18
                                       t
Finding t
 Solu on (Con nued)



      20 = 80e− 5 ln 4 + 18
                 t
Finding t
 Solu on (Con nued)



      20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4
                 t                        t
Finding t
 Solu on (Con nued)


                                                     1
      20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 =⇒      = e− 5 ln 4
                t                       t                   t

                                                    40
Finding t
 Solu on (Con nued)


                                                     1
      20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 =⇒      = e− 5 ln 4
                t                       t                   t

                                                    40
             t
  − ln 40 = − ln 4
             5
Finding t
 Solu on (Con nued)


                                                     1
      20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 =⇒      = e− 5 ln 4
                t                       t                   t

                                                    40
             t            ln 40    5 ln 40
  − ln 40 = − ln 4 =⇒ t = 1      =         ≈ 13 min
             5            5 ln 4     ln 4
Computing time of death with NLC
Example
A murder vic m is discovered at
midnight and the temperature of the
body is recorded as 31 ◦ C. One hour
later, the temperature of the body is
29 ◦ C. Assume that the surrounding
air temperature remains constant at
21 ◦ C. Calculate the vic m’s me of
death. (The “normal” temperature of
a living human being is approximately
37 ◦ C.)
Solu on
   Let me 0 be midnight. We know T0 = 31, Ts = 21, and
   T(1) = 29. We want to know the t for which T(t) = 37.
Solu on
   Let me 0 be midnight. We know T0 = 31, Ts = 21, and
   T(1) = 29. We want to know the t for which T(t) = 37.
   To find k:

                 29 = 10ek·1 + 21 =⇒ k = ln 0.8
Solu on
   Let me 0 be midnight. We know T0 = 31, Ts = 21, and
   T(1) = 29. We want to know the t for which T(t) = 37.
   To find k:

                  29 = 10ek·1 + 21 =⇒ k = ln 0.8

   To find t:

               37 = 10et·ln(0.8) + 21 =⇒ 1.6 = et·ln(0.8)
                    ln(1.6)
                t=            ≈ −2.10 hr
                    ln(0.8)
   So the me of death was just before 10:00      .
Outline
 Recall
 The differen al equa on y′ = ky
 Modeling simple popula on growth
 Modeling radioac ve decay
   Carbon-14 Da ng
 Newton’s Law of Cooling
 Con nuously Compounded Interest
Interest
   If an account has an compound interest rate of r per year
   compounded n mes, then an ini al deposit of A0 dollars
   becomes                   (     r )nt
                           A0 1 +
                                   n
   a er t years.
Interest
   If an account has an compound interest rate of r per year
   compounded n mes, then an ini al deposit of A0 dollars
   becomes                    (    r )nt
                            A0 1 +
                                   n
   a er t years.
   For different amounts of compounding, this will change. As
   n → ∞, we get con nously compounded interest
                                (    r )nt
                  A(t) = lim A0 1 +        = A0 ert .
                         n→∞         n
Interest
   If an account has an compound interest rate of r per year
   compounded n mes, then an ini al deposit of A0 dollars
   becomes                    (    r )nt
                            A0 1 +
                                   n
   a er t years.
   For different amounts of compounding, this will change. As
   n → ∞, we get con nously compounded interest
                                (    r )nt
                  A(t) = lim A0 1 +        = A0 ert .
                         n→∞         n

   Thus dollars are like bacteria.
Continuous vs. Discrete Compounding of interest
  Example
  Consider two bank accounts: one with 10% annual interested compounded
  quarterly and one with annual interest rate r compunded con nuously. If they
  produce the same balance a er every year, what is r?
Continuous vs. Discrete Compounding of interest
  Example
  Consider two bank accounts: one with 10% annual interested compounded
  quarterly and one with annual interest rate r compunded con nuously. If they
  produce the same balance a er every year, what is r?

  Solu on
  The balance for the 10% compounded quarterly account a er t years
  is
                  A1 (t) = A0 (1.025)4t = A0 ((1.025)4 )t
  The balance for the interest rate r compounded con nuously
  account a er t years is
                              A2 (t) = A0 ert
Solving
 Solu on (Con nued)


                        A1 (t) = A0 ((1.025)4 )t
                        A2 (t) = A0 (er )t

 For those to be the same, er = (1.025)4 , so

               r = ln((1.025)4 ) = 4 ln 1.025 ≈ 0.0988

 So 10% annual interest compounded quarterly is basically equivalent
 to 9.88% compounded con nuously.
Computing doubling time
 Example
 How long does it take an ini al deposit of $100, compounded
 con nuously, to double?
Computing doubling time
 Example
 How long does it take an ini al deposit of $100, compounded
 con nuously, to double?

 Solu on
 We need t such that A(t) = 200. In other words
                                                         ln 2
      200 = 100ert =⇒ 2 = ert =⇒ ln 2 = rt =⇒ t =             .
                                                           r
 For instance, if r = 6% = 0.06, we have
                     ln 2   0.69 69
                t=        ≈     =   = 11.5 years.
                     0.06 0.06    6
I-banking interview tip of the day
                 ln 2
   The frac on        can also be
                   r
   approximated as either 70 or 72
   divided by the percentage rate
   (as a number between 0 and
   100, not a frac on between 0
   and 1.)
   This is some mes called the rule
   of 70 or rule of 72.
   72 has lots of factors so it’s used
   more o en.
Summary

  When something grows or decays at a constant rela ve rate,
  the growth or decay is exponen al.
  Equa ons with unknowns in an exponent can be solved with
  logarithms.
  Your friend list is like culture of bacteria (no offense).

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Exponential Growth and Radioactive Decay

  • 1. Sec on 3.4 Exponen al Growth and Decay V63.0121.011: Calculus I Professor Ma hew Leingang New York University March 23, 2011 .
  • 2. Announcements Quiz 3 next week in recita on on 2.6, 2.8, 3.1, 3.2
  • 3. Objectives Solve the ordinary differen al equa on y′ (t) = ky(t), y(0) = y0 Solve problems involving exponen al growth and decay
  • 4. Outline Recall The differen al equa on y′ = ky Modeling simple popula on growth Modeling radioac ve decay Carbon-14 Da ng Newton’s Law of Cooling Con nuously Compounded Interest
  • 5. Derivatives of exponential and logarithmic functions y y′ ex ex ax (ln a) · ax 1 ln x x 1 1 loga x · ln a x
  • 6. Outline Recall The differen al equa on y′ = ky Modeling simple popula on growth Modeling radioac ve decay Carbon-14 Da ng Newton’s Law of Cooling Con nuously Compounded Interest
  • 7. What is a differential equation? Defini on A differen al equa on is an equa on for an unknown func on which includes the func on and its deriva ves.
  • 8. What is a differential equation? Defini on A differen al equa on is an equa on for an unknown func on which includes the func on and its deriva ves. Example Newton’s Second Law F = ma is a differen al equa on, where a(t) = x′′ (t).
  • 9. What is a differential equation? Defini on A differen al equa on is an equa on for an unknown func on which includes the func on and its deriva ves. Example Newton’s Second Law F = ma is a differen al equa on, where a(t) = x′′ (t). In a spring, F(x) = −kx, where x is displacement from equilibrium and k is a constant. So k −kx(t) = mx′′ (t) =⇒ x′′ (t) + x(t) = 0. m
  • 10. Showing a function is a solution Example (Con nued) Show that x(t) = A sin ωt + B cos ωt sa sfies the differen al k √ equa on x′′ + x = 0, where ω = k/m. m
  • 11. Showing a function is a solution Example (Con nued) Show that x(t) = A sin ωt + B cos ωt sa sfies the differen al k √ equa on x′′ + x = 0, where ω = k/m. m Solu on We have x(t) = A sin ωt + B cos ωt x′ (t) = Aω cos ωt − Bω sin ωt x′′ (t) = −Aω 2 sin ωt − Bω 2 cos ωt
  • 12. The Equation y′ = 2 Example Find a solu on to y′ (t) = 2. Find the most general solu on to y′ (t) = 2.
  • 13. The Equation y′ = 2 Example Find a solu on to y′ (t) = 2. Find the most general solu on to y′ (t) = 2. Solu on A solu on is y(t) = 2t.
  • 14. The Equation y′ = 2 Example Find a solu on to y′ (t) = 2. Find the most general solu on to y′ (t) = 2. Solu on A solu on is y(t) = 2t. The general solu on is y = 2t + C.
  • 15. The Equation y′ = 2 Example Find a solu on to y′ (t) = 2. Find the most general solu on to y′ (t) = 2. Solu on A solu on is y(t) = 2t. The general solu on is y = 2t + C. Remark If a func on has a constant rate of growth, it’s linear.
  • 16. The Equation y′ = 2t Example Find a solu on to y′ (t) = 2t. Find the most general solu on to y′ (t) = 2t.
  • 17. The Equation y′ = 2t Example Find a solu on to y′ (t) = 2t. Find the most general solu on to y′ (t) = 2t. Solu on A solu on is y(t) = t2 .
  • 18. The Equation y′ = 2t Example Find a solu on to y′ (t) = 2t. Find the most general solu on to y′ (t) = 2t. Solu on A solu on is y(t) = t2 . The general solu on is y = t2 + C.
  • 19. The Equation y′ = y Example Find a solu on to y′ (t) = y(t). Find the most general solu on to y′ (t) = y(t).
  • 20. The Equation y′ = y Example Find a solu on to y′ (t) = y(t). Find the most general solu on to y′ (t) = y(t). Solu on A solu on is y(t) = et .
  • 21. The Equation y′ = y Example Find a solu on to y′ (t) = y(t). Find the most general solu on to y′ (t) = y(t). Solu on A solu on is y(t) = et . The general solu on is y = Cet , not y = et + C. (check this)
  • 22. Kick it up a notch: y′ = 2y Example Find a solu on to y′ = 2y. Find the general solu on to y′ = 2y.
  • 23. Kick it up a notch: y′ = 2y Example Find a solu on to y′ = 2y. Find the general solu on to y′ = 2y. Solu on y = e2t y = Ce2t
  • 24. In general: y′ = ky Example Find a solu on to y′ = ky. Find the general solu on to y′ = ky.
  • 25. In general: y′ = ky Example Find a solu on to y′ = ky. Find the general solu on to y′ = ky. Solu on y = ekt y = Cekt
  • 26. In general: y′ = ky Example Find a solu on to y′ = ky. Find the general solu on to y′ = ky. Solu on Remark y = ekt What is C? Plug in t = 0: y = Cekt y(0) = Cek·0 = C · 1 = C, so y(0) = y0 , the ini al value of y.
  • 27. Constant Relative Growth =⇒ Exponential Growth Theorem A func on with constant rela ve growth rate k is an exponen al func on with parameter k. Explicitly, the solu on to the equa on y′ (t) = ky(t) y(0) = y0 is y(t) = y0 ekt
  • 28. Exponential Growth is everywhere Lots of situa ons have growth rates propor onal to the current value This is the same as saying the rela ve growth rate is constant. Examples: Natural popula on growth, compounded interest, social networks
  • 29. Outline Recall The differen al equa on y′ = ky Modeling simple popula on growth Modeling radioac ve decay Carbon-14 Da ng Newton’s Law of Cooling Con nuously Compounded Interest
  • 30. Bacteria Since you need bacteria to make bacteria, the amount of new bacteria at any moment is propor onal to the total amount of bacteria. This means bacteria popula ons grow exponen ally.
  • 31. Bacteria Example Example A colony of bacteria is grown under ideal condi ons in a laboratory. At the end of 3 hours there are 10,000 bacteria. At the end of 5 hours there are 40,000. How many bacteria were present ini ally?
  • 32. Bacteria Example Example A colony of bacteria is grown under ideal condi ons in a laboratory. At the end of 3 hours there are 10,000 bacteria. At the end of 5 hours there are 40,000. How many bacteria were present ini ally? Solu on Since y′ = ky for bacteria, we have y = y0 ekt . We have 10, 000 = y0 ek·3 40, 000 = y0 ek·5
  • 33. Bacteria Example Solution Solu on (Con nued) We have 10, 000 = y0 ek·3 40, 000 = y0 ek·5 Dividing the first into the second gives 40, 000 y0 e5k = 3k =⇒ 4 = e2k =⇒ ln 4 = ln(e2k ) = 2k 10, 000 y0 e ln 4 ln 22 2 ln 2 =⇒ k = = = = ln 2 2 2 2
  • 34. Solu on (Con nued) Since y = y0 et ln 2 , at me t = 3 we have 10, 000 10, 000 = y0 e3 ln 2 = y0 · 8 =⇒ y0 = = 1250 8
  • 35. Outline Recall The differen al equa on y′ = ky Modeling simple popula on growth Modeling radioac ve decay Carbon-14 Da ng Newton’s Law of Cooling Con nuously Compounded Interest
  • 36. Modeling radioactive decay Radioac ve decay occurs because many large atoms spontaneously give off par cles.
  • 37. Modeling radioactive decay Radioac ve decay occurs because many large atoms spontaneously give off par cles. This means that in a sample of a bunch of atoms, we can assume a certain percentage of them will “go off” at any point. (For instance, if all atom of a certain radioac ve element have a 20% chance of decaying at any point, then we can expect in a sample of 100 that 20 of them will be decaying.)
  • 38. Radioactive decay as a differential equation The rela ve rate of decay is constant: y′ =k y where k is nega ve.
  • 39. Radioactive decay as a differential equation The rela ve rate of decay is constant: y′ =k y where k is nega ve. So y′ = ky =⇒ y = y0 ekt again!
  • 40. Radioactive decay as a differential equation The rela ve rate of decay is constant: y′ =k y where k is nega ve. So y′ = ky =⇒ y = y0 ekt again! It’s customary to express the rela ve rate of decay in the units of half-life: the amount of me it takes a pure sample to decay to one which is only half pure.
  • 41. Computing the amount remaining Example The half-life of polonium-210 is about 138 days. How much of a 100 g sample remains a er t years?
  • 42. Computing the amount remaining Example The half-life of polonium-210 is about 138 days. How much of a 100 g sample remains a er t years? Solu on We have y = y0 ekt , where y0 = y(0) = 100 grams. Then 365 · ln 2 50 = 100ek·138/365 =⇒ k = − . 138 Therefore y(t) = 100e− = 100 · 2−365t/138 365·ln 2 138 t
  • 43. Computing the amount remaining Example The half-life of polonium-210 is about 138 days. How much of a 100 g sample remains a er t years? Solu on We have y = y0 ekt , where y0 = y(0) = 100 grams. Then 365 · ln 2 50 = 100ek·138/365 =⇒ k = − . 138 Therefore y(t) = 100e− = 100 · 2−365t/138 365·ln 2 138 t
  • 44. Carbon-14 Dating The ra o of carbon-14 to carbon-12 in an organism decays exponen ally: p(t) = p0 e−kt . The half-life of carbon-14 is about 5700 years. So the equa on for p(t) is p(t) = p0 e− 5700 t = p0 2−t/5700 ln2
  • 45. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil?
  • 46. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solu on p(t) We are looking for the value of t for which = 0.1. p0
  • 47. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solu on p(t) We are looking for the value of t for which = 0.1. From the equa on we have p0 2−t/5700 = 0.1
  • 48. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solu on p(t) We are looking for the value of t for which = 0.1. From the equa on we have p0 t 2−t/5700 = 0.1 =⇒ − ln 2 = ln 0.1 5700
  • 49. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solu on p(t) We are looking for the value of t for which = 0.1. From the equa on we have p0 t ln 0.1 2−t/5700 = 0.1 =⇒ − ln 2 = ln 0.1 =⇒ t = · 5700 5700 ln 2
  • 50. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solu on p(t) We are looking for the value of t for which = 0.1. From the equa on we have p0 t ln 0.1 2−t/5700 = 0.1 =⇒ − ln 2 = ln 0.1 =⇒ t = · 5700 ≈ 18, 940 5700 ln 2
  • 51. Computing age with Carbon-14 Example Suppose a fossil is found where the ra o of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solu on p(t) We are looking for the value of t for which = 0.1. From the equa on we have p0 t ln 0.1 2−t/5700 = 0.1 =⇒ − ln 2 = ln 0.1 =⇒ t = · 5700 ≈ 18, 940 5700 ln 2 So the fossil is almost 19,000 years old.
  • 52. Outline Recall The differen al equa on y′ = ky Modeling simple popula on growth Modeling radioac ve decay Carbon-14 Da ng Newton’s Law of Cooling Con nuously Compounded Interest
  • 53. Newton’s Law of Cooling Newton’s Law of Cooling states that the rate of cooling of an object is propor onal to the temperature difference between the object and its surroundings.
  • 54. Newton’s Law of Cooling Newton’s Law of Cooling states that the rate of cooling of an object is propor onal to the temperature difference between the object and its surroundings. This gives us a differen al equa on of the form dT = k(T − Ts ) dt (where k < 0 again).
  • 55. General Solution to NLC problems ′ ′ To solve this, change the variable y(t) = T(t) − Ts . Then y = T and k(T − Ts ) = ky. The equa on now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt
  • 56. General Solution to NLC problems ′ ′ To solve this, change the variable y(t) = T(t) − Ts . Then y = T and k(T − Ts ) = ky. The equa on now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt Now we can solve! y′ = ky
  • 57. General Solution to NLC problems ′ ′ To solve this, change the variable y(t) = T(t) − Ts . Then y = T and k(T − Ts ) = ky. The equa on now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt Now we can solve! y′ = ky =⇒ y = Cekt
  • 58. General Solution to NLC problems ′ ′ To solve this, change the variable y(t) = T(t) − Ts . Then y = T and k(T − Ts ) = ky. The equa on now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt Now we can solve! y′ = ky =⇒ y = Cekt =⇒ T − Ts = Cekt
  • 59. General Solution to NLC problems ′ ′ To solve this, change the variable y(t) = T(t) − Ts . Then y = T and k(T − Ts ) = ky. The equa on now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt Now we can solve! y′ = ky =⇒ y = Cekt =⇒ T − Ts = Cekt =⇒ T = Cekt + Ts
  • 60. General Solution to NLC problems ′ ′ To solve this, change the variable y(t) = T(t) − Ts . Then y = T and k(T − Ts ) = ky. The equa on now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt Now we can solve! y′ = ky =⇒ y = Cekt =⇒ T − Ts = Cekt =⇒ T = Cekt + Ts Plugging in t = 0, we see C = y0 = T0 − Ts . So Theorem The solu on to the equa on T′ (t) = k(T(t) − Ts ), T(0) = T0 is T(t) = (T0 − Ts )ekt + Ts
  • 61. Computing cooling time with NLC Example A hard-boiled egg at 98 ◦ C is put in a sink of 18 ◦ C water. A er 5 minutes, the egg’s temperature is 38 ◦ C. Assuming the water has not warmed appreciably, how much longer will it take the egg to reach 20 ◦ C?
  • 62. Computing cooling time with NLC Example A hard-boiled egg at 98 ◦ C is put in a sink of 18 ◦ C water. A er 5 minutes, the egg’s temperature is 38 ◦ C. Assuming the water has not warmed appreciably, how much longer will it take the egg to reach 20 ◦ C? Solu on We know that the temperature func on takes the form T(t) = (T0 − Ts )ekt + Ts = 80ekt + 18 To find k, plug in t = 5 and solve for k.
  • 63. Finding k Solu on (Con nued) 38 = T(5) = 80e5k + 18
  • 64. Finding k Solu on (Con nued) 38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k
  • 65. Finding k Solu on (Con nued) 38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k 1 = e5k 4
  • 66. Finding k Solu on (Con nued) 38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k ( ) 1 1 = e5k =⇒ ln = 5k 4 4
  • 67. Finding k Solu on (Con nued) 38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k ( ) 1 1 1 = e5k =⇒ ln = 5k =⇒ k = − ln 4. 4 4 5
  • 68. Finding k Solu on (Con nued) 38 = T(5) = 80e5k + 18 =⇒ 20 = 80e5k ( ) 1 1 1 = e5k =⇒ ln = 5k =⇒ k = − ln 4. 4 4 5 Now we need to solve for t: 20 = T(t) = 80e− 5 ln 4 + 18 t
  • 69. Finding t Solu on (Con nued) 20 = 80e− 5 ln 4 + 18 t
  • 70. Finding t Solu on (Con nued) 20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 t t
  • 71. Finding t Solu on (Con nued) 1 20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 =⇒ = e− 5 ln 4 t t t 40
  • 72. Finding t Solu on (Con nued) 1 20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 =⇒ = e− 5 ln 4 t t t 40 t − ln 40 = − ln 4 5
  • 73. Finding t Solu on (Con nued) 1 20 = 80e− 5 ln 4 + 18 =⇒ 2 = 80e− 5 ln 4 =⇒ = e− 5 ln 4 t t t 40 t ln 40 5 ln 40 − ln 40 = − ln 4 =⇒ t = 1 = ≈ 13 min 5 5 ln 4 ln 4
  • 74. Computing time of death with NLC Example A murder vic m is discovered at midnight and the temperature of the body is recorded as 31 ◦ C. One hour later, the temperature of the body is 29 ◦ C. Assume that the surrounding air temperature remains constant at 21 ◦ C. Calculate the vic m’s me of death. (The “normal” temperature of a living human being is approximately 37 ◦ C.)
  • 75. Solu on Let me 0 be midnight. We know T0 = 31, Ts = 21, and T(1) = 29. We want to know the t for which T(t) = 37.
  • 76. Solu on Let me 0 be midnight. We know T0 = 31, Ts = 21, and T(1) = 29. We want to know the t for which T(t) = 37. To find k: 29 = 10ek·1 + 21 =⇒ k = ln 0.8
  • 77. Solu on Let me 0 be midnight. We know T0 = 31, Ts = 21, and T(1) = 29. We want to know the t for which T(t) = 37. To find k: 29 = 10ek·1 + 21 =⇒ k = ln 0.8 To find t: 37 = 10et·ln(0.8) + 21 =⇒ 1.6 = et·ln(0.8) ln(1.6) t= ≈ −2.10 hr ln(0.8) So the me of death was just before 10:00 .
  • 78. Outline Recall The differen al equa on y′ = ky Modeling simple popula on growth Modeling radioac ve decay Carbon-14 Da ng Newton’s Law of Cooling Con nuously Compounded Interest
  • 79. Interest If an account has an compound interest rate of r per year compounded n mes, then an ini al deposit of A0 dollars becomes ( r )nt A0 1 + n a er t years.
  • 80. Interest If an account has an compound interest rate of r per year compounded n mes, then an ini al deposit of A0 dollars becomes ( r )nt A0 1 + n a er t years. For different amounts of compounding, this will change. As n → ∞, we get con nously compounded interest ( r )nt A(t) = lim A0 1 + = A0 ert . n→∞ n
  • 81. Interest If an account has an compound interest rate of r per year compounded n mes, then an ini al deposit of A0 dollars becomes ( r )nt A0 1 + n a er t years. For different amounts of compounding, this will change. As n → ∞, we get con nously compounded interest ( r )nt A(t) = lim A0 1 + = A0 ert . n→∞ n Thus dollars are like bacteria.
  • 82. Continuous vs. Discrete Compounding of interest Example Consider two bank accounts: one with 10% annual interested compounded quarterly and one with annual interest rate r compunded con nuously. If they produce the same balance a er every year, what is r?
  • 83. Continuous vs. Discrete Compounding of interest Example Consider two bank accounts: one with 10% annual interested compounded quarterly and one with annual interest rate r compunded con nuously. If they produce the same balance a er every year, what is r? Solu on The balance for the 10% compounded quarterly account a er t years is A1 (t) = A0 (1.025)4t = A0 ((1.025)4 )t The balance for the interest rate r compounded con nuously account a er t years is A2 (t) = A0 ert
  • 84. Solving Solu on (Con nued) A1 (t) = A0 ((1.025)4 )t A2 (t) = A0 (er )t For those to be the same, er = (1.025)4 , so r = ln((1.025)4 ) = 4 ln 1.025 ≈ 0.0988 So 10% annual interest compounded quarterly is basically equivalent to 9.88% compounded con nuously.
  • 85. Computing doubling time Example How long does it take an ini al deposit of $100, compounded con nuously, to double?
  • 86. Computing doubling time Example How long does it take an ini al deposit of $100, compounded con nuously, to double? Solu on We need t such that A(t) = 200. In other words ln 2 200 = 100ert =⇒ 2 = ert =⇒ ln 2 = rt =⇒ t = . r For instance, if r = 6% = 0.06, we have ln 2 0.69 69 t= ≈ = = 11.5 years. 0.06 0.06 6
  • 87. I-banking interview tip of the day ln 2 The frac on can also be r approximated as either 70 or 72 divided by the percentage rate (as a number between 0 and 100, not a frac on between 0 and 1.) This is some mes called the rule of 70 or rule of 72. 72 has lots of factors so it’s used more o en.
  • 88. Summary When something grows or decays at a constant rela ve rate, the growth or decay is exponen al. Equa ons with unknowns in an exponent can be solved with logarithms. Your friend list is like culture of bacteria (no offense).