6.1 Antiderivatives with Slope Fields Consider: then: y x2 3 y x2 5 or y 2 x y 2 x It doesn’t matter whether the constant was 3 or -5, since when we take the derivative the constant disappears. However, when we try to reverse the operation: Given: y 2 x y x2 C find y We don’t know what the constant is, so we put “C” in the answer to remind us that there might have been a constant. 6.1 Antiderivatives with Slope Fields Given: y 2 x and y 4 when x 1 , find the equation for y . y x2 C 4 12 C 3C y x2 3 This is called an initial value problem. We need the initial values to find the constant. An equation containing a derivative is called a differential equation. It becomes an initial value problem when you are given the initial condition and asked to find the original equation. 6.1 Antiderivatives with Slope Fields Definition Slope Field or Directional Field A slope field or a directional field for the first order differentiable equation dy f ( x, y ) dx is a plot of sort line segments with slopes f(x,y) for a lattice of points (x,y) in the plane. Initial value problems and differential equations can be illustrated with a slope field. 6.1 Antiderivatives with Slope Fields y 2 x x y y' 0 0 0 1 0 2 0 3 1 0 1 1 2 0 -1 0 -2 0 0 0 0 0 2 2 4 -2 -4 6.1 Antiderivatives with Slope Fields y 2 x If you know an initial condition, such as (1,-2), you can sketch the curve. By following the slope field, you get a rough picture of what the curve looks like. In this case, it is a parabola. 6.1 Antiderivatives with Slope Fields 4 1 2 Integrals such as x dx 4 1 4 1 3 x C 3 1 x dx are called definite integrals because we can find a definite value for the answer. 1 3 1 3 4 C 1 C 3 3 64 1 C C 3 3 2 63 3 The constant always cancels when finding a definite integral, so we leave it out! 21 6.1 Antiderivatives with Slope Fields Integrals such as x dx 2 are called indefinite integrals because we can not find a definite value for the answer. 2 x dx 1 3 x C 3 When finding indefinite integrals, we always include the “plus C”. 6.1 Antiderivatives with Slope Fields Definition Indefinite Integral The set of all antiderivatives of a function f(x) is the indefinite integral of f with respect to x and is denoted by f ( x)dx f ( x)dx F ( x) C 6.1 Antiderivatives with Slope Fields 1. x dx n dx 2. x x n1 C , n 1 n 1 ln x C 3. e dx e C x x 4. sin x dx cos x C 6.1 Antiderivatives with Slope Fields 5. cos x dx sin x C 6. sec x dx tan x C 7. csc x dx cot x C 8. sec x tan x dx sec x C 2 2 9. csc x cot x dx csc x C 6.1 Antiderivatives with Slope Fields (x x 3 3 2 x 3)dx x dx 1 t 2 cos t dt 4 x 2 x 3x C 4 9 2 2 x C 9 1 sin t C t 6.1 Antiderivatives with Slope Fields sec x(tan x cos x)dx sec x x C (1 sin x cos x C (e 2t 2 x csc x) dx t ) dt 2 e 2t t 3 C 2 3 6.1 Antiderivatives with Slope Fields Find the position function for v(t) = t3 - 2t2 + t s(0) = 1 4 3 2 t 2t t s(t ) C 4 3 2 4 3 2 0 2(0) (0) 1 C 4 3 2 4 3 2 t 2t t s(t ) 1 4 3 2 C=1 6.1 Antiderivatives with Slope Fields d (cabin ) cabin log cabin + C log cabin houseboat 6.2 Integration by Substitution The chain rule allows us to differentiate a wide variety of functions, but we are able to find antiderivatives for only a limited range of functions. We can sometimes use substitution to rewrite functions in a form that we can integrate. 6.2 Integration by Substitution x 2 5 dx u du Let u x 2 du dx 5 1 6 u C 6 x 2 6 6 C The variable of integration must match the variable in the expression. Don’t forget to substitute the value for u back into the problem! 6.2 Integration by Substitution 1 x 2 x dx 2 u 1 2 1 x 2 Let u 1 x du 2 x dx 2 The derivative of du 3 2 2 u C 3 One of the clues that we look for is if we can find a function and its derivative in the integrand. 2 1 x 3 3 2 2 C is 2x dx . Note that this only worked because of the 2x in the original. Many integrals can not be done by substitution. 6.2 Integration by Substitution 4 x 1 dx Let u 4x 1 du 4 dx 1 2 1 u 4 du 3 2 1 du dx 4 2 1 u C 3 4 3 2 1 u C 6 3 1 4 x 1 2 C 6 Solve for dx. 6.2 Integration by Substitution cos 7 x 5 dx 1 cos u 7 du 1 sin u C 7 1 sin 7 x 5 C 7 Let u 7 x 5 du 7 dx 1 du dx 7 6.2 Integration by Substitution 2 3 x sin x dx 1 sin u du 3 1 cos u C 3 1 3 cos x C 3 Let u x3 du 3x 2 dx 1 du x 2 dx 3 2 We solve for x dx because we can find it in the integrand. 6.2 Integration by Substitution sin 4 x cos x dx sin x 4 u du 4 cos x dx 1 5 u C 5 1 5 sin x C 5 Let u sin x du cos x dx 6.2 Integration by Substitution 4 0 2 tan x sec x dx new limit 1 u du 0 new limit 1 1 2 u 2 0 1 2 The technique is a little different for definite integrals. Let u tan x 2 du sec x dx We can find new limits, u 0 tan 0 0 and then we don’t have u tan 1 to substitute 4 4 back. We could have substituted back and used the original limits. 6.2 Integration by Substitution 4 0 Using the original limits: tan x sec2 x dx du sec x dx 4 0 Let u tan x 2 u du u du 1 1 2 tan tan 0 2 4 2 Wrong! 2 Leave the limits out until you substitute back. 1 2 u 2 1 2 4 tan x 2 0 This is The match! 1 limits 1 don’t usually 2 2 1 1 0 more work 2 2 2 than finding new limits 6.2 Integration by Substitution 1 1 2 0 3x 2 x 1 dx 3 Let u x3 1 du 3x dx 2 1 2 u du 2 u 3 3 2 2 2 2 3 u 1 2 Don’t forget to use the new limits. 0 3 2 u 1 0 2 2 2 3 4 2 3 6.2 Integration by Substitution 2 x 1 x dx 2 3x 4 dx t 5 3t dt 2 8 tan t dt 3 sin cos d cot csc 2 d 6.2 Integration by Substitution x2 dx x 1 5 2 4 5x e 3 e5 x dx cos x sin 2 x dx dx 0 e dx x ln x 1 x x 2 dx 1 x 2 e2 e 6.2 Integration by Substitution In another generation or so, we might be able to use the calculator to find all integrals. Until then, remember that half the AP exam and half the nation’s college professors do not allow calculators. You must practice finding integrals by hand until you are good at it! 6.3 Integrating by Parts Start with the product rule: d dv du uv u v dx dx dx d uv u dv v du d uv v du u dv u dv d uv v du u dv d uv v du u dv d uv v du u dv uv v du This is the Integration by Parts formula. 6.3 Integrating by Parts u dv uv v du u differentiates to dv is easy to zero (usually). integrate. The Integration by Parts formula is a “product rule” for integration. Choose u in this order: LIPET Logs, Inverse trig, Polynomial, Exponential, Trig 6.3 Integrating by Parts x cos x dx polynomial factor u v v du x sin x sin x dx u dv uv v du LIPET ux dv cos x dx du dx v sin x x sin x cos x C 6.3 Integrating by Parts ln x dx logarithmic factor u v v du 1 ln x x x dx x u dv uv v du LIPET u ln x dv dx 1 du dx x vx x ln x x C 6.3 Integrating by Parts x e dx u v v du x e e 2 x dx 2 x 2 x u dv uv v du x x x e 2 xe e dx 2 x x u x2 dv e x dx du 2 x dx v ex ux x e 2 xe dx 2 x LIPET x dv e x dx This is still a product, so x we v e du dx need to use integration by parts again. x e 2 xe 2e C 2 x x x 6.3 Integrating by Parts A Shortcut: Tabular Integration Tabular integration works for integrals of the form: f x g x dx where: Differentiates to zero in several steps. Integrates repeatedly. Also called tic-tac-toe method 6.3 Integrating by Parts 2 x x e dx f x & deriv. g x & integrals 2 x ex 2x e x 2 ex 0 ex Compare this with the same problem done the other way: x 2 x x 2 e x e 2 xe C x e dx 2 x 6.3 Integrating by Parts x 3 sin x dx 3 x 3x 2 sin x cos x 6x 6 sin x cos x 0 sin x x 3 cos x 3x 2 sin x 6x cos x 6sin x + C 6.3 Integrating by Parts LIPET e x u cos x cos x dx u v v du cos x e x e x sin x dx cos x e x e x sin x dx du sin x dx v ex u sin x dv e x dx du cos x dx cos x e sin x e e cos x dx x x x dv e dx x ve x This is the expression we started with! 6.3 Integrating by Parts e x u cos x dv e dx x du sin x dx v e x cos x dx cos x e x e x sin x dx cos x e x e x sin x dx x u sin x dv e dx du cos x dx v e x e cos x dx cos x e sin x e e 2 e cos x dx cos x e sin x e sin x e cos x e C e cos x dx 2 x x x x x x x x x x cos x dx 6.3 Integrating by Parts The goal of integrating by parts is to go from an integral u dv that we don’t see how to integrate to an integral v du that we can evaluate. 6.4 Exponential Growth and Decay The number of rabbits in a population increases at a rate that is proportional to the number of rabbits present (at least for awhile.) So does any population of living creatures. Other things that increase or decrease at a rate proportional to the amount present include radioactive material and money in an interest-bearing account. If the rate of change is proportional to the amount present, dy the change can be modeled by: dt ky 6.4 Exponential Growth and Decay dy ky dt 1 dy k dt y 1 y dy k dt ln y kt C Rate of change is proportional to the amount present. Divide both sides by y. Integrate both sides. 6.4 Exponential Growth and Decay ln y e e kt C y e e C kt Exponentiate both sides. When multiplying like bases, add exponents. So added exponents can be written as multiplication. 6.4 Exponential Growth and Decay y e e C kt y Ae kt y0 Ae y0 A Since eC is a constant, let e C A. 1 k 0 At t 0 , y y0 y y0 e kt . This is the solution to our original initial value problem. 6.4 Exponential Growth and Decay Exponential Change: y y0 e kt If the constant k is positive then the equation represents growth. If k is negative then the equation represents decay. 6.4 Exponential Growth and Decay Continuously Compounded Interest If money is invested in a fixed-interest account where the interest is added to the account k times per year, the kt r amount present after t years is: A t A0 1 k If the money is added back more frequently, you will make a little more money. The best you can do is if the interest is added continuously. 6.4 Exponential Growth and Decay Of course, the bank does not employ some clerk to continuously calculate your interest with an adding machine. We could calculate: r lim A0 1 k k kt Since the interest is proportional to the amount present, the equation becomes: Continuously Compounded Interest: A A0e rt You may also use: A Pe rt which is the same thing. 6.4 Exponential Growth and Decay Radioactive Decay The equation for the amount of a radioactive element left after time t is: y yO e kt The half-life is the time required for half the material to decay. 6.4 Exponential Growth and Decay Radioactive Decay 60 mg of radon, half-life of 1690 years. How much is left after 100 years? y yO e kt 30 60e1690k 1 e1690k 2 1 ln 1690k 2 k .00041 y 60e ( .00041)(100) y 58 mg 6.4 Exponential Growth and Decay 100 bacteria are present initially and double every 12 minutes. How long before there are 1,000,000 y yO e kt 200 100e 12 k k .0577 1,000,000 100e(.0577)(t ) 2e 10000 e.0577t ln 2 12k t 159 minutes 12 k 6.4 Exponential Growth and Decay 1 kt y0 y0 e 2 1 ln ln e kt 2 0 ln1 ln 2 kt Half-life Half-life: ln 2 kt ln 2 t k ln 2 half-life k 6.4 Exponential Growth and Decay Espresso left in a cup will cool to the temperature of the surrounding air. The rate of cooling is proportional to the difference in temperature between the liquid and the air. dT If we solve the k T Ts differential equation: dt Newton’s Law of Cooling we get: T Ts T0 Ts e kt where Ts is the temperature of the surrounding medium, which is a constant. 6.5 Population Growth 100 80 60 Bears 40 20 0 20 40 Years 60 80 100 6.5 Population Growth kt y y e We have used the exponential growth equation 0 to represent population growth. The exponential growth equation occurs when the rate of growth is proportional to the amount present. If we use P to represent the population, the differential equation becomes: dP / dt dP kP dt The constant k is called the relative growth rate. P k 6.5 Population Growth kt P P e The population growth model becomes: 0 However, real-life populations do not increase forever. There is some limiting factor such as food, living space or waste disposal. There is a maximum population, or carrying capacity, M. 6.5 Population Growth A more realistic model is the logistic growth model where growth rate is proportional to both the amount present (P) and the fraction of the carrying capacity that remains: M P M 6.5 Population Growth The equation then becomes: dP M P kP dt M Logistics Differential Equation Our book writes it this way: dP k P M P dt M We can solve this differential equation to find the logistics growth model. 6.5 Population Growth Logistics Differential Equation dP k P M P dt M 1 k dP dt P M P M 1 1 1 k dt dP M P M P M ln P ln M P kt C P ln kt C M P 1 A B P M P P M P 1 A M P BP 1 AM AP BP 1 AM 1 A M Partial Fractions 0 AP BP AP BP AB 1 B M 6.5 Population Growth Logistics Differential Equation dP k P M P dt M 1 k dP dt P M P M 1 1 1 k dt dP M P M P M ln P ln M P kt C P ln kt C M P P e kt C M P M P e kt C P M 1 e kt C P M 1 e kt C P 6.5 Population Growth Logistics Differential Equation P e kt C M P M P e kt C P M 1 e kt C P M 1 e kt C P M P 1 e kt C P M 1 e C e kt Let A e C M P 1 Ae kt 6.5 Population Growth Logistics Growth Model M P 1 Ae kt 6.5 Population Growth Logistic Growth Model Ten grizzly bears were introduced to a national park 10 years ago. There are 23 bears in the park at the present time. The park can support a maximum of 100 bears. Assuming a logistic growth model, when will the bear population reach 50? 75? 100? 6.5 Population Growth Ten grizzly bears were introduced to a national park 10 years ago. There are 23 bears in the park at the present time. The park can support a maximum of 100 bears. Assuming a logistic growth model, when will the bear population reach 50? 75? 100? M P 1 Ae kt M 100 P0 10 P10 23 6.5 Population Growth M P 1 Ae kt M 100 100 10 1 Ae0 At time zero, the population is 10. P0 10 P10 23 10 A 90 100 10 1 A 10 10 A 100 A9 100 P 1 9e kt 6.5 Population Growth M P 1 Ae kt M 100 100 23 1 9e k 10 100 1 9e 23 77 10 k 9e 23 e10 k 0.371981 10 k 100 P0 10 P10 23 P 1 9e kt After 10 years, the population is 23. 10k 0.988913 k 0.098891 100 P 1 9e 0.1t 6.5 Population Growth 100 100 P 1 9e 0.1t We can graph this equation and use “trace” to find the solutions. 80 60 Bears 40 20 0 y=50 at 22 years 20 40 Years y=75 at 33 years 60 80 100 y=100 at 75 years 6.6 Euler’s Method Leonhard Euler made a huge number of contributions to mathematics, almost half after he was totally blind. (When this portrait was made he had already lost most of the sight in his right eye.) Leonhard Euler 1707 - 1783 6.6 Euler’s Method It was Euler who originated the following notations: f x (function notation) e (base of natural log) (pi) i (summation) y 1 (finite change) Leonhard Euler 1707 - 1783 6.6 Euler’s Method There are many differential equations that can not be solved. We can still find an approximate solution. We will practice with an easy one that can be solved. dy 2x dx Initial value: y0 1 6.6 Euler’s Method Recall the formula for local linearization L( x) y( x0 ) y' ( x0 )dx y1 y0 f ( x0 , y0 )dx where dy f ( x, y ) dx 6.6 Euler’s Method dy 2x dx y0 1 dx 0.5 y1 y0 f ( x0 , y0 )dx (0,1) y1 1 (0)(.5) 1 (.5,1) y2 y1 f ( x1, y1 )dx y2 1 (1)(.5) 1.5 5 4 3 2 (1,1.5) 1 0 1 2 3 6.6 Euler’s Method y3 y2 f ( x2 , y2 )dx y3 1.5 (2)(.5) 2.5 5 (1.5,2.5) 3 y4 y3 f ( x3 , y3 )dx y4 2.5 (3)(.5) 4 4 2 (2,4) 1 0 1 2 3 6.6 Euler’s Method 5 Exact Solution: dy 2x dx dy 2 x dx 0,1 dx 0.5 4 3 y x2 C 2 1 1 0C y x2 1 0 1 2 3 6.6 Euler’s Method This is called Euler’s Method. 5 4 It is more accurate if a smaller value is used for dx. It gets less accurate as you move away from the initial value. 3 2 1 0 1 2 3 6.6 Euler’s Method The book refers to an “Improved Euler’s Method”. We will not be using it, and you do not need to know it. The calculator also contains a similar but more complicated (and more accurate) formula called the Runge-Kutta method. You don’t need to know anything about it other than the fact that it is used more often in real life. This is the RK solution method on your calculator.