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_Why_Slopes_&_More_Math_1995

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Volume 3,  Why Slopes and More Math 


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 For better work & study skills, read chapters 2  in  Three Skills for Algebra. Sooner is better. Good luck.

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Online Volume 2, Three Skills for Algebra, Chapters 1 to 25 - skip 18., verbalizes and explains key skills and concepts, those needed in calculus, again to make the hard easier. A visual understanding of complex numbers may serve as back ground info for partial fraction decomposition.

Area Calculation Problem

The selection of labels x and y for the horizontal and vertical axes for most of graphs met so far is arbitrary. It can be changed. The letters s and q could have been used instead in all the previous graphs. You should imagine this replacement, and the effect, if any, it has on your knowledge or opinion of mathematics.

 

 

Problem: Suppose G(x) and h(x) are continuous at each point x in the interval [a,b]. Further suppose that the slope G¢(x) of G(x) satisfies G¢(x) = h(x) for a £ x £ b. Find a formula for the area A under the curve q = h(s) between s = a and s = b.
The solution to this problem follows in three steps.

Step 1. Define an Area Function

First, introduce a function F(x) as follows. For each x between a and b inclusive let
F(x) = (Area from s = a to s = x)


Here F(a) = 0 and F(b) = A is the area to be computed. Note that the area computation will be based on (a) finding the slope or derivative F¢(x) and then (b) observing how to obtain F(x) from a knowledge of F¢(x). The value of A = F(b) is required. It will be given by a formula involving the function G(x).

Step 2. Area Function Slope Calculation

Second, the following diagram leads to a formula for F¢(x).


In this figure, the area under q = h(s) from s = x to s = x+Dx is given by
DF = F(x+Dx)-F(x) » h(x)Dx
and hence
F(x+Dx)-F(x)
Dx
» h(x)
These approximations are expected (hoped?) to improve when Dx® 0 approaches zero. This hope or expectation suggests that
F¢(x) =
lim
Dx ®
DF
Dx
=
lim
Dx ®
F(x+Dx)-F(x)
Dx
= h(x)
Therefore the derivative or slope function for F(x) should be
F¢(x) = h(x)
This formula gives the rate of change of area F(x) for each given value of x. The small print below provides a more refined argument to justify the assertion that F¢(x) = h(x).


Since h(s) is assumed to be continuous on the interval [a,b], it is continuous at the point s1 = x. Therefore, for every whole number k, there is a number n such that
|h(s)-h(x)| £ 1
2
·10-k
when |s-x| £ [1/2]·10-n. Now given k and such an n, if x £ s £ x+Dx and 0 £ Dx £ [1/2]·10-n then |s-x| £ |Dx| £ [1/2]·10-n as well. For such numbers s, it follows that |h(s)-h(x)| £ [1/2]·10-k. The latter in turn (see diagram) implies that the region B [between q = h(x) and q = h(s) above the s-interval from s = x to s = x+Dx] has an area
|Area B| = |F(x+Dx) -F(x) -h(x)Dx| £ Dx · 1
2
·10-k
This is equivalent to
ê
ê
ê
Area B
Dx
ê
ê
ê
= ê
ê
ê
|F(x+Dx) -F(x) -h(x)Dx
Dx
ê
ê
ê
£ 1
2
·10-k
Therefore
ê
ê
ê
Area B
Dx
ê
ê
ê
= ê
ê
ê
F(x+Dx) -F(x)
Dx
 - h(x) ê
ê
ê
£ 1
2
·10-k
when 0 £ Dx £ [1/2]·10-n. Since the foregoing argument holds for every whole number k > 0, it implies that the limiting value of [(F(x+Dx) -F(x))/(Dx)] = h(x) when Dx > 0 approaches zero.

Step 3. Difference of Two Functions

Third, the previous discussion of vertical motions (and earthquakes) implies or suggests that for x in the interval [a,b], the difference F(x)-G(x) = C for some constant number C which does not depend on x. Recall F(a) = 0. This implies C = F(a)-G(a) = 0-G(a) = -G(a). Therefore, the constant value is given by C = -G(a) because F(a) = 0. Now F(x)-G(x) = C implies
F(x) = G(x)+C = G(x)+(-G(a)) = G(x)-G(a)
Therefore F(x) = G(x)-G(a) and the sought-after are
A = F(b) = G(b)-G(a)

Remark.   The latter formula is correct whenever G(x) is a function whose slope or derivative is h(x) for every x in the interval [a,b]. Given a formula for the function h(s) or h(x), the area calculation problem can be solved easily if methods of anti-differentiation can provide a G(x). For some h(x), this is possible. In particular, methods for anti-differentiation can be employed (sometimes) to find several functions G(x) whose derivative or slope on the interval x = a to x = b coincides everywhere with the slope h¢(x) of F(x). The problem statement above assumed one such function G(x) was available.

 


Methods for anti-differentiation or reversing slope calculations say how to find possible formulas for a function f(x) from a single formula for its derivative (slope) m = f¢(x). These methods are ad hoc. They do not work in all examples, but they do work in a large number. Methods for finding or obtaining a function from its derivative or slope lead to formulas for the calculation of areas, volumes, weights, masses, forces, totals etc met in geometrical, physical and some business computations.

Remark.   The computation of many geometric, physical and business quantities can be related to the computation of the area under the graph of some function q = h(s). The unit of area in these graphs is given by a product of the units of the horizontal and vertical coordinates q and s.

 

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Volume 3,  Why Slopes and More Math 


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For  help in calculus, explore
Volumes
2. Three Skills for Algebra and 3. Why Slopes & More Math, and  Calculus Introduction site area. See how to learn or teach key skills and concepts, some not all.

Foreword, One Calculus  preview and Online Chapters: (V) signals video (RealPlayer Format)  to watch 

Area Intro
Foreword
Chapter Descriptions
1. Introduction
Cal. Preview (1983  lesson why slopes)
2. Second Preview Begins
2 Skier in Motion (V)
2 The Skier (V)
2. Position Dependent (V)
3 Slope & Extrema (V)
4 Single Factor Analysis (V)
4 Two Factor (V)
4 More Factors (V)
4 With Divisors (V)
5 Maxima & Minima Tests
6 Jumps & Discontinuities
8 Review  (optional)
9 On Calculus Studies
11 Slope of Slope
13  Acceleration
14 Limits & Error Control (V)
14 Limit of a Fn.
14. Limited Error Control
14 Signif. Digits
14 Cauchy Limits
14 Sequence Limits
14 Decimal Arith.
15 What is Slope (V)
15 Slope Calculation (V)
15 Slope, a Limit
15 Tangent Lines
15 Linear Approx.,
15 Limits via Algebra (V)
15 Recap.
PS.Chain Rule for Polys
PS Chain Rule- General  (V) -
PS More Chain Rule (V)
PS - Sign Analysis (V)
16 What is Velocity
17  What is Area
18 Integration
18 Area Calculation
18  Fn DefN, 6 Ways
19 Logs & Powers
19 Natural Log.
19 Exponential Fn.
20 What's Next
21 Add Vectors
22 Complex #'s
23 Complex #'s
23 Trig Identity
23 Proofs of.
24 Complex Logs etc

Units in Calculations:
7 Velocity
7 Varying Velocity Example
7. Velocity Calculation
7 Changing Units
7 Same Velocity  Motions
10 Slopes without Units.
10 Units & Slopes
10  Units in Cost vs. Quantity
10  How Units  Appear
10 Unit  Elimination
10 Partial Elimination
10 Interest & Units
12 More on Units
Content Guide

Enriched material: The Appendices of Volume 3 are located in the Real  Analysis  Area.

Pigeon Hole Principle
Constant Difference Thm
Continuous Functions
Rational Functions
Mean Value Theorem
One Side Range Theorem
Range On One Side Theorem
Integration & Lipschitz
 Continuity


These appendices continue the
decimal viewpoint of limits, error
control and continuity begun
in Chapter 14. The One Sided
 Range Theorem
is a postscript,
not in printed version.



 

 


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