Section	3.4
     Exponential	Growth	and	Decay

                V63.0121.006/016, Calculus	I



                       March	10, 2010


Announcements
   Midterm	is	(almost)	graded, will	be	returned	in	recitation
   Scores	and	grades	will	be	massaged
   We	will	drop	the	five	lowest	WebAssign-ments
                                           .   .    .    .      .   .
Announcements




     Midterm	is	(almost)	graded, will	be	returned	in	recitation
     Scores	and	grades	will	be	massaged
     We	will	drop	the	five	lowest	WebAssign-ments




                                             .   .    .    .      .   .
Outline

  Recall

  The	equation y′ = ky

  Modeling	simple	population	growth

  Modeling	radioactive	decay
    Carbon-14	Dating

  Newton’s	Law	of	Cooling

  Continuously	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	equation y′ = ky

  Modeling	simple	population	growth

  Modeling	radioactive	decay
    Carbon-14	Dating

  Newton’s	Law	of	Cooling

  Continuously	Compounded	Interest



                                      .   .   .   .   .   .
Definition
A differential	equation is	an	equation	for	an	unknown	function
which	includes	the	function	and	its	derivatives.




                                           .   .    .   .   .    .
Definition
A differential	equation is	an	equation	for	an	unknown	function
which	includes	the	function	and	its	derivatives.

Example
    Newton’s	Second	Law F = ma is	a	differential	equation,
    where a(t) = x′′ (t).




                                           .   .    .   .    .   .
Definition
A differential	equation is	an	equation	for	an	unknown	function
which	includes	the	function	and	its	derivatives.

Example
    Newton’s	Second	Law F = ma is	a	differential	equation,
    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




                                               .      .    .     .   .   .
Definition
A differential	equation is	an	equation	for	an	unknown	function
which	includes	the	function	and	its	derivatives.

Example
    Newton’s	Second	Law F = ma is	a	differential	equation,
    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


    The	most	general	solution	is x(t) = A sin ω t + B cos ω t, where
        √
    ω = k/m.


                                               .      .    .     .   .   .
The	Equation y′ = 2t



   Example
      Find a solution	to y′ (t) = 2t.
      Find	the most	general solution	to y′ (t) = 2t.




                                               .       .   .   .   .   .
The	Equation y′ = 2t



   Example
       Find a solution	to y′ (t) = 2t.
       Find	the most	general solution	to y′ (t) = 2t.

   Solution
       A solution	is y(t) = t2 .




                                                .       .   .   .   .   .
The	Equation y′ = 2t



   Example
       Find a solution	to y′ (t) = 2t.
       Find	the most	general solution	to y′ (t) = 2t.

   Solution
       A solution	is y(t) = t2 .
       The	general	solution	is y = t2 + C.
   (check	this)




                                                .       .   .   .   .   .
The	equation y′ = ky



   Example
      Find a solution	to y′ (t) = y(t).
      Find	the most	general solution	to y′ (t) = y(t).




                                               .    .    .   .   .   .
The	equation y′ = ky



   Example
       Find a solution	to y′ (t) = y(t).
       Find	the most	general solution	to y′ (t) = y(t).

   Solution
       A solution	is y(t) = et .




                                                .    .    .   .   .   .
The	equation y′ = ky



   Example
       Find a solution	to y′ (t) = y(t).
       Find	the most	general solution	to y′ (t) = y(t).

   Solution
       A solution	is y(t) = et .
       The	general	solution	is y = Cet , not y = et + C.
   (check	this)




                                                .    .     .   .   .   .
Kick	it	up	a	notch



   Example
      Find	a	solution	to y′ = 2y.
      Find	the	general	solution	to y′ = 2y.




                                              .   .   .   .   .   .
Kick	it	up	a	notch



   Example
       Find	a	solution	to y′ = 2y.
       Find	the	general	solution	to y′ = 2y.

   Solution
       y = e2t
       y = Ce2t




                                               .   .   .   .   .   .
In	general

   Example
      Find	a	solution	to y′ = ky.
      Find	the	general	solution	to y′ = ky.




                                              .   .   .   .   .   .
In	general

   Example
       Find	a	solution	to y′ = ky.
       Find	the	general	solution	to y′ = ky.

   Solution
       y = ekt
       y = Cekt




                                               .   .   .   .   .   .
In	general

   Example
        Find	a	solution	to y′ = ky.
        Find	the	general	solution	to y′ = ky.

   Solution
        y = ekt
        y = Cekt

   Remark
   What	is C? Plug	in t = 0:

                         y(0) = Cek·0 = C · 1 = C,

   so y(0) = y0 , the initial	value of y.
                                                .    .   .   .   .   .
Exponential	Growth


      It	means	the	rate	of	change	(derivative)	is	proportional	to	the
      current	value
      Examples: Natural	population	growth, compounded	interest,
      social	networks




                                               .   .    .    .    .     .
Outline

  Recall

  The	equation y′ = ky

  Modeling	simple	population	growth

  Modeling	radioactive	decay
    Carbon-14	Dating

  Newton’s	Law	of	Cooling

  Continuously	Compounded	Interest



                                      .   .   .   .   .   .
Bacteria



     Since	you	need	bacteria
     to	make	bacteria, the
     amount	of	new	bacteria
     at	any	moment	is
     proportional	to	the	total
     amount	of	bacteria.
     This	means	bacteria
     populations	grow
     exponentially.




                                 .   .   .   .   .   .
Bacteria	Example
  Example
  A colony	of	bacteria	is	grown	under	ideal	conditions	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	initially?




                                              .    .   .    .   .   .
Bacteria	Example
  Example
  A colony	of	bacteria	is	grown	under	ideal	conditions	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	initially?

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

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




                                               .   .    .    .   .   .
Bacteria	Example
  Example
  A colony	of	bacteria	is	grown	under	ideal	conditions	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	initially?

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

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

  Dividing	the	first	into	the	second	gives
  4 = e2k =⇒ 2k = ln 4 =⇒ k = ln 2. Now	we	have

                     10, 000 = y0 eln 2·3 = y0 · 8

            10, 000
  So y0 =           = 1250.
               8
                                               .     .   .   .   .   .
Could	you	do	that	again	please?

   We	have

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

   Dividing	the	first	into	the	second	gives

                 40, 000  y e5k
                         = 0 3k
                 10, 000  y0 e
                  =⇒ 4 = e2k
                =⇒ ln 4 = ln(e2k ) = 2k
                            ln 4   ln 22   2 ln 2
                  =⇒ k =         =       =        = ln 2
                             2       2        2


                                               .   .       .   .   .   .
Outline

  Recall

  The	equation y′ = ky

  Modeling	simple	population	growth

  Modeling	radioactive	decay
    Carbon-14	Dating

  Newton’s	Law	of	Cooling

  Continuously	Compounded	Interest



                                      .   .   .   .   .   .
Modeling	radioactive	decay

   Radioactive	decay	occurs	because	many	large	atoms
   spontaneously	give	off	particles.




                                            .   .      .   .   .   .
Modeling	radioactive	decay

   Radioactive	decay	occurs	because	many	large	atoms
   spontaneously	give	off	particles.

  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	radioactive
  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.)


                                            .   .      .   .   .   .
Thus	the	relative	rate	of	decay	is	constant:

                               y′
                                  =k
                               y

where k is negative.




                                               .   .   .   .   .   .
Thus	the	relative	rate	of	decay	is	constant:

                               y′
                                  =k
                               y

where k is negative. So

                      y′ = ky =⇒ y = y0 ekt

again!




                                               .   .   .   .   .   .
Thus	the	relative	rate	of	decay	is	constant:

                               y′
                                  =k
                               y

where k is negative. So

                      y′ = ky =⇒ y = y0 ekt

again!
It’s	customary	to	express	the	relative	rate	of	decay	in	the	units	of
half-life: the	amount	of	time	it	takes	a	pure	sample	to	decay	to
one	which	is	only	half	pure.




                                               .   .    .    .    .    .
Example
The	half-life	of	polonium-210	is	about	138	days. How	much	of	a
100	g	sample	remains	after t years?




                                          .   .   .    .   .     .
Example
The	half-life	of	polonium-210	is	about	138	days. How	much	of	a
100	g	sample	remains	after t years?

Solution
We	have y = y0 ekt , where y0 = y(0) = 100 grams. Then

                                                   365 · ln 2
            50 = 100ek·138/365 =⇒ k = −                       .
                                                     138
Therefore
                            365·ln 2
             y(t) = 100e−     138
                                     t
                                         = 100 · 2−365t/138 .




                                                    .    .      .   .   .   .
Example
The	half-life	of	polonium-210	is	about	138	days. How	much	of	a
100	g	sample	remains	after t years?

Solution
We	have y = y0 ekt , where y0 = y(0) = 100 grams. Then

                                                     365 · ln 2
             50 = 100ek·138/365 =⇒ k = −                        .
                                                       138
Therefore
                              365·ln 2
               y(t) = 100e−     138
                                       t
                                           = 100 · 2−365t/138 .

Notice y(t) = y0 · 2−t/t1/2 , where t1/2 is	the	half-life.



                                                      .    .      .   .   .   .
Carbon-14	Dating

                   The	ratio	of	carbon-14	to
                   carbon-12	in	an	organism
                   decays	exponentially:

                              p(t) = p0 e−kt .

                   The	half-life	of	carbon-14	is
                   about	5700	years. So	the
                   equation	for p(t) is
                                           ln2
                          p(t) = p0 e− 5700 t

                   Another	way	to	write	this
                   would	be

                         p(t) = p0 2−t/5700

                          .       .    .    .    .   .
Example
Suppose	a	fossil	is	found	where	the	ratio	of	carbon-14	to
carbon-12	is	10%	of	that	in	a	living	organism. How	old	is	the
fossil?




                                           .    .   .    .      .   .
Example
Suppose	a	fossil	is	found	where	the	ratio	of	carbon-14	to
carbon-12	is	10%	of	that	in	a	living	organism. How	old	is	the
fossil?

Solution
We	are	looking	for	the	value	of t for	which

                           p(t)
                                = 0.1
                           p(0)




                                              .   .   .   .     .   .
Example
Suppose	a	fossil	is	found	where	the	ratio	of	carbon-14	to
carbon-12	is	10%	of	that	in	a	living	organism. How	old	is	the
fossil?

Solution
We	are	looking	for	the	value	of t for	which

                           p(t)
                                = 0.1
                           p(0)

From	the	equation	we	have

                         2−t/5700 = 0.1
                          t
                      −        ln 2 = ln 0.1
                        5700
                      ln 0.1
                   t=        · 5700 ≈ 18, 940
                       ln 2

                                              .   .   .   .     .   .
Example
Suppose	a	fossil	is	found	where	the	ratio	of	carbon-14	to
carbon-12	is	10%	of	that	in	a	living	organism. How	old	is	the
fossil?

Solution
We	are	looking	for	the	value	of t for	which

                            p(t)
                                 = 0.1
                            p(0)

From	the	equation	we	have

                         2−t/5700 = 0.1
                          t
                      −        ln 2 = ln 0.1
                        5700
                      ln 0.1
                   t=        · 5700 ≈ 18, 940
                       ln 2
So	the	fossil	is	almost	19,000	years	old.
                                              .   .   .   .     .   .
Outline

  Recall

  The	equation y′ = ky

  Modeling	simple	population	growth

  Modeling	radioactive	decay
    Carbon-14	Dating

  Newton’s	Law	of	Cooling

  Continuously	Compounded	Interest



                                      .   .   .   .   .   .
Newton’s	Law	of	Cooling

     Newton’s	Law	of
     Cooling states	that	the
     rate	of	cooling	of	an
     object	is	proportional	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	proportional	to
     the	temperature
     difference	between	the
     object	and	its
     surroundings.
     This	gives	us	a
     differential	equation	of
     the	form
          dT
             = k (T − T s )
          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	equation	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	equation	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	equation	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

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


                                                .   .    .    .   .    .
Example
A hard-boiled	egg	at 98◦ C is	put	in	a	sink	of 18◦ C water. After	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?




                                             .    .   .    .    .     .
Example
A hard-boiled	egg	at 98◦ C is	put	in	a	sink	of 18◦ C water. After	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?

Solution
We	know	that	the	temperature	function	takes	the	form

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

To	find k, plug	in t = 5:

                     38 = T(5) = 80e5k + 18

and	solve	for k.


                                             .    .    .   .    .     .
Finding k


                38 = T(5) = 80e5k + 18
                 20 = 80e5k
                  1
                    = e5k
               ( )4
                1
            ln      = 5k
                4
                        1
              =⇒ k = − ln 4.
                        5




                                   .     .   .   .   .   .
Finding k


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

   for t.
                                             .     .   .   .   .   .
Finding t



                            t
                20 = 80e− 5 ln 4 + 18
                            t
                  2 = 80e− 5 ln 4
                 1       t
                    = e− 5 ln 4
                40
                        t
            − ln 40 = − ln 4
                        5

                       ln 40    5 ln 40
             =⇒ t =    1
                              =         ≈ 13 min
                       5 ln 4     ln 4




                                         .   .     .   .   .   .
Example
A murder	victim	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	victim’s	time	of	death.
(The	“normal”	temperature	of
a	living	human	being	is
approximately 37 ◦ C.)


                                 .   .   .   .   .   .
Solution
    Let	time 0 be	midnight. We	know T0 = 31, Ts = 21, and
    T(1) = 29. We	want	to	know	the t for	which T(t) = 37.




                                         .   .   .   .      .   .
Solution
    Let	time 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




                                         .   .   .   .      .   .
Solution
    Let	time 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	time	of	death	was	just	before	10:00pm.

                                              .    .   .   .   .   .
Outline

  Recall

  The	equation y′ = ky

  Modeling	simple	population	growth

  Modeling	radioactive	decay
    Carbon-14	Dating

  Newton’s	Law	of	Cooling

  Continuously	Compounded	Interest



                                      .   .   .   .   .   .
Interest

       If	an	account	has	an	compound	interest	rate	of r per	year
       compounded n times, then	an	initial	deposit	of A0 dollars
       becomes                  (     r )nt
                              A0 1 +
                                     n
       after t years.




                                              .   .    .   .   .   .
Interest

       If	an	account	has	an	compound	interest	rate	of r per	year
       compounded n times, then	an	initial	deposit	of A0 dollars
       becomes                  (     r )nt
                              A0 1 +
                                     n
       after t years.
       For	different	amounts	of	compounding, this	will	change. As
       n → ∞, we	get continously	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 times, then	an	initial	deposit	of A0 dollars
       becomes                  (     r )nt
                              A0 1 +
                                     n
       after t years.
       For	different	amounts	of	compounding, this	will	change. As
       n → ∞, we	get continously	compounded	interest
                                 (    r )nt
                    A(t) = lim A0 1 +       = A0 ert .
                          n→∞         n


       Thus	dollars	are	like	bacteria.


                                              .   .      .   .   .   .
Example
How	long	does	it	take	an	initial	deposit	of	$100, compounded
continuously, to	double?




                                          .   .    .   .   .   .
Example
How	long	does	it	take	an	initial	deposit	of	$100, compounded
continuously, to	double?

Solution
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	fraction      can
                    r
     also	be	approximated	as
     either	70	or	72	divided
     by	the	percentage	rate
     (as	a	number	between	0
     and	100, not	a	fraction
     between	0	and	1.)
     This	is	sometimes	called
     the rule	of	70 or rule	of
     72.
     72	has	lots	of	factors	so
     it’s	used	more	often.


                                     .   .   .   .   .   .
What	have	we	learned	today?




      When	something	grows	or	decays	at	a	constant relative rate,
      the	growth	or	decay	is	exponential.
      Equations	with	unknowns	in	an	exponent	can	be	solved	with
      logarithms.
      Your	friend	list	is	like	culture	of	bacteria	(no	offense).




                                                 .    .    .       .   .   .

Lesson 14: Exponential Growth and Decay

  • 1.
    Section 3.4 Exponential Growth and Decay V63.0121.006/016, Calculus I March 10, 2010 Announcements Midterm is (almost) graded, will be returned in recitation Scores and grades will be massaged We will drop the five lowest WebAssign-ments . . . . . .
  • 2.
    Announcements Midterm is (almost) graded, will be returned in recitation Scores and grades will be massaged We will drop the five lowest WebAssign-ments . . . . . .
  • 3.
    Outline Recall The equation y′ = ky Modeling simple population growth Modeling radioactive decay Carbon-14 Dating Newton’s Law of Cooling Continuously Compounded Interest . . . . . .
  • 4.
    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 . . . . . .
  • 5.
    Outline Recall The equation y′ = ky Modeling simple population growth Modeling radioactive decay Carbon-14 Dating Newton’s Law of Cooling Continuously Compounded Interest . . . . . .
  • 6.
  • 7.
    Definition A differential equation is an equation for an unknown function which includes the function and its derivatives. Example Newton’s Second Law F = ma is a differential equation, where a(t) = x′′ (t). . . . . . .
  • 8.
    Definition A differential equation is an equation for an unknown function which includes the function and its derivatives. Example Newton’s Second Law F = ma is a differential equation, 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 . . . . . .
  • 9.
    Definition A differential equation is an equation for an unknown function which includes the function and its derivatives. Example Newton’s Second Law F = ma is a differential equation, 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 The most general solution is x(t) = A sin ω t + B cos ω t, where √ ω = k/m. . . . . . .
  • 10.
    The Equation y′ =2t Example Find a solution to y′ (t) = 2t. Find the most general solution to y′ (t) = 2t. . . . . . .
  • 11.
    The Equation y′ =2t Example Find a solution to y′ (t) = 2t. Find the most general solution to y′ (t) = 2t. Solution A solution is y(t) = t2 . . . . . . .
  • 12.
    The Equation y′ =2t Example Find a solution to y′ (t) = 2t. Find the most general solution to y′ (t) = 2t. Solution A solution is y(t) = t2 . The general solution is y = t2 + C. (check this) . . . . . .
  • 13.
    The equation y′ =ky Example Find a solution to y′ (t) = y(t). Find the most general solution to y′ (t) = y(t). . . . . . .
  • 14.
    The equation y′ =ky Example Find a solution to y′ (t) = y(t). Find the most general solution to y′ (t) = y(t). Solution A solution is y(t) = et . . . . . . .
  • 15.
    The equation y′ =ky Example Find a solution to y′ (t) = y(t). Find the most general solution to y′ (t) = y(t). Solution A solution is y(t) = et . The general solution is y = Cet , not y = et + C. (check this) . . . . . .
  • 16.
    Kick it up a notch Example Find a solution to y′ = 2y. Find the general solution to y′ = 2y. . . . . . .
  • 17.
    Kick it up a notch Example Find a solution to y′ = 2y. Find the general solution to y′ = 2y. Solution y = e2t y = Ce2t . . . . . .
  • 18.
    In general Example Find a solution to y′ = ky. Find the general solution to y′ = ky. . . . . . .
  • 19.
    In general Example Find a solution to y′ = ky. Find the general solution to y′ = ky. Solution y = ekt y = Cekt . . . . . .
  • 20.
    In general Example Find a solution to y′ = ky. Find the general solution to y′ = ky. Solution y = ekt y = Cekt Remark What is C? Plug in t = 0: y(0) = Cek·0 = C · 1 = C, so y(0) = y0 , the initial value of y. . . . . . .
  • 21.
    Exponential Growth It means the rate of change (derivative) is proportional to the current value Examples: Natural population growth, compounded interest, social networks . . . . . .
  • 22.
    Outline Recall The equation y′ = ky Modeling simple population growth Modeling radioactive decay Carbon-14 Dating Newton’s Law of Cooling Continuously Compounded Interest . . . . . .
  • 23.
    Bacteria Since you need bacteria to make bacteria, the amount of new bacteria at any moment is proportional to the total amount of bacteria. This means bacteria populations grow exponentially. . . . . . .
  • 24.
    Bacteria Example Example A colony of bacteria is grown under ideal conditions 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 initially? . . . . . .
  • 25.
    Bacteria Example Example A colony of bacteria is grown under ideal conditions 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 initially? Solution Since y′ = ky for bacteria, we have y = y0 ekt . We have 10, 000 = y0 ek·3 40, 000 = y0 ek·5 . . . . . .
  • 26.
    Bacteria Example Example A colony of bacteria is grown under ideal conditions 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 initially? Solution Since y′ = ky for bacteria, we have y = y0 ekt . We have 10, 000 = y0 ek·3 40, 000 = y0 ek·5 Dividing the first into the second gives 4 = e2k =⇒ 2k = ln 4 =⇒ k = ln 2. Now we have 10, 000 = y0 eln 2·3 = y0 · 8 10, 000 So y0 = = 1250. 8 . . . . . .
  • 27.
    Could you do that again please? We have 10, 000 = y0 ek·3 40, 000 = y0 ek·5 Dividing the first into the second gives 40, 000 y e5k = 0 3k 10, 000 y0 e =⇒ 4 = e2k =⇒ ln 4 = ln(e2k ) = 2k ln 4 ln 22 2 ln 2 =⇒ k = = = = ln 2 2 2 2 . . . . . .
  • 28.
    Outline Recall The equation y′ = ky Modeling simple population growth Modeling radioactive decay Carbon-14 Dating Newton’s Law of Cooling Continuously Compounded Interest . . . . . .
  • 29.
    Modeling radioactive decay Radioactive decay occurs because many large atoms spontaneously give off particles. . . . . . .
  • 30.
    Modeling radioactive decay Radioactive decay occurs because many large atoms spontaneously give off particles. 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 radioactive 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.) . . . . . .
  • 31.
    Thus the relative rate of decay is constant: y′ =k y where k is negative. . . . . . .
  • 32.
    Thus the relative rate of decay is constant: y′ =k y where k is negative. So y′ = ky =⇒ y = y0 ekt again! . . . . . .
  • 33.
    Thus the relative rate of decay is constant: y′ =k y where k is negative. So y′ = ky =⇒ y = y0 ekt again! It’s customary to express the relative rate of decay in the units of half-life: the amount of time it takes a pure sample to decay to one which is only half pure. . . . . . .
  • 34.
  • 35.
    Example The half-life of polonium-210 is about 138 days. How much of a 100 g sample remains after tyears? Solution We have y = y0 ekt , where y0 = y(0) = 100 grams. Then 365 · ln 2 50 = 100ek·138/365 =⇒ k = − . 138 Therefore 365·ln 2 y(t) = 100e− 138 t = 100 · 2−365t/138 . . . . . . .
  • 36.
    Example The half-life of polonium-210 is about 138 days. How much of a 100 g sample remains after tyears? Solution We have y = y0 ekt , where y0 = y(0) = 100 grams. Then 365 · ln 2 50 = 100ek·138/365 =⇒ k = − . 138 Therefore 365·ln 2 y(t) = 100e− 138 t = 100 · 2−365t/138 . Notice y(t) = y0 · 2−t/t1/2 , where t1/2 is the half-life. . . . . . .
  • 37.
    Carbon-14 Dating The ratio of carbon-14 to carbon-12 in an organism decays exponentially: p(t) = p0 e−kt . The half-life of carbon-14 is about 5700 years. So the equation for p(t) is ln2 p(t) = p0 e− 5700 t Another way to write this would be p(t) = p0 2−t/5700 . . . . . .
  • 38.
  • 39.
  • 40.
    Example Suppose a fossil is found where the ratio of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solution We are looking for the value of tfor which p(t) = 0.1 p(0) From the equation we have 2−t/5700 = 0.1 t − ln 2 = ln 0.1 5700 ln 0.1 t= · 5700 ≈ 18, 940 ln 2 . . . . . .
  • 41.
    Example Suppose a fossil is found where the ratio of carbon-14 to carbon-12 is 10% of that in a living organism. How old is the fossil? Solution We are looking for the value of tfor which p(t) = 0.1 p(0) From the equation we have 2−t/5700 = 0.1 t − ln 2 = ln 0.1 5700 ln 0.1 t= · 5700 ≈ 18, 940 ln 2 So the fossil is almost 19,000 years old. . . . . . .
  • 42.
    Outline Recall The equation y′ = ky Modeling simple population growth Modeling radioactive decay Carbon-14 Dating Newton’s Law of Cooling Continuously Compounded Interest . . . . . .
  • 43.
    Newton’s Law of Cooling Newton’s Law of Cooling states that the rate of cooling of an object is proportional to the temperature difference between the object and its surroundings. . . . . . .
  • 44.
    Newton’s Law of Cooling Newton’s Law of Cooling states that the rate of cooling of an object is proportional to the temperature difference between the object and its surroundings. This gives us a differential equation of the form dT = k (T − T s ) dt (where k < 0 again). . . . . . .
  • 45.
    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 equation now looks like dT dy = k(T − Ts ) ⇐⇒ = ky dt dt . . . . . .
  • 46.
    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 equation 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 . . . . . .
  • 47.
    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 equation 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 T(t) = (T0 − Ts )ekt + Ts . . . . . .
  • 48.
    Example A hard-boiled egg at 98◦C is put in a sink of 18◦ C water. After 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? . . . . . .
  • 49.
    Example A hard-boiled egg at 98◦C is put in a sink of 18◦ C water. After 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? Solution We know that the temperature function takes the form T(t) = (T0 − Ts )ekt + Ts = 80ekt + 18 To find k, plug in t = 5: 38 = T(5) = 80e5k + 18 and solve for k. . . . . . .
  • 50.
    Finding k 38 = T(5) = 80e5k + 18 20 = 80e5k 1 = e5k ( )4 1 ln = 5k 4 1 =⇒ k = − ln 4. 5 . . . . . .
  • 51.
    Finding k 38 = T(5) = 80e5k + 18 20 = 80e5k 1 = e5k ( )4 1 ln = 5k 4 1 =⇒ k = − ln 4. 5 Now we need to solve t 20 = T(t) = 80e− 5 ln 4 + 18 for t. . . . . . .
  • 52.
    Finding t t 20 = 80e− 5 ln 4 + 18 t 2 = 80e− 5 ln 4 1 t = e− 5 ln 4 40 t − ln 40 = − ln 4 5 ln 40 5 ln 40 =⇒ t = 1 = ≈ 13 min 5 ln 4 ln 4 . . . . . .
  • 53.
    Example A murder victim 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 victim’s time of death. (The “normal” temperature of a living human being is approximately 37 ◦ C.) . . . . . .
  • 54.
    Solution Let time 0 be midnight. We know T0 = 31, Ts = 21, and T(1) = 29. We want to know the t for which T(t) = 37. . . . . . .
  • 55.
    Solution Let time 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 . . . . . .
  • 56.
    Solution Let time 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 time of death was just before 10:00pm. . . . . . .
  • 57.
    Outline Recall The equation y′ = ky Modeling simple population growth Modeling radioactive decay Carbon-14 Dating Newton’s Law of Cooling Continuously Compounded Interest . . . . . .
  • 58.
    Interest If an account has an compound interest rate of r per year compounded n times, then an initial deposit of A0 dollars becomes ( r )nt A0 1 + n after t years. . . . . . .
  • 59.
    Interest If an account has an compound interest rate of r per year compounded n times, then an initial deposit of A0 dollars becomes ( r )nt A0 1 + n after t years. For different amounts of compounding, this will change. As n → ∞, we get continously compounded interest ( r )nt A(t) = lim A0 1 + = A0 ert . n→∞ n . . . . . .
  • 60.
    Interest If an account has an compound interest rate of r per year compounded n times, then an initial deposit of A0 dollars becomes ( r )nt A0 1 + n after t years. For different amounts of compounding, this will change. As n → ∞, we get continously compounded interest ( r )nt A(t) = lim A0 1 + = A0 ert . n→∞ n Thus dollars are like bacteria. . . . . . .
  • 61.
  • 62.
    Example How long does it take an initial deposit of $100, compounded continuously, to double? Solution We needt 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 . . . . . .
  • 63.
    I-banking interview tip of the day ln 2 The fraction can r also be approximated as either 70 or 72 divided by the percentage rate (as a number between 0 and 100, not a fraction between 0 and 1.) This is sometimes called the rule of 70 or rule of 72. 72 has lots of factors so it’s used more often. . . . . . .
  • 64.
    What have we learned today? When something grows or decays at a constant relative rate, the growth or decay is exponential. Equations with unknowns in an exponent can be solved with logarithms. Your friend list is like culture of bacteria (no offense). . . . . . .