Chapter 5 addressed the problem of creating an accumulation function in open form when we have its rate of change at every moment as a function in closed form. In the next chapter we will start from where we ended in Chapter 5. In this chapter, we addressed the first foundational problem of calculus:
Let $dx$ and $dy$ vary over each $\Delta x$-sized interval. Approximations to the exact accumulation over intervals are then continuous. Each value of $dx$ produces a value of $dy=m dx$ as $dx$ varies, thus defining the approximate net accumulation functionA as a piecewise linear function that approximates the exact net accumulationfunction $A_f$. The meaning of $A_f(x)$ is that any value of $A_f(x)$ is the net accumulation (variation) in the value of f from an initial value a to any value of x.
When $\Delta x$ is so small that making it smaller has no appreciable effect on our estimates of the net accumulation from a to x, we said $A_f$ was the exact net accumulationfunction for $r_f$. We represented $A_f$ in open form as $A_f(x) = \int_a^x r(t)dt$.
The relationship between $A_f$ and f is that for any given value of a, $A_f(x)=f(x)-f(a)$. Said another way, every value of $A_f(x)$ gives us the net variation in f from a to x, and the net variation in f from a to x is $f(x)-f(a)$.
Therefore $f(x) = f(a) + A_f(x)$, which says that $f(x)$—the accumulation in f up to a value of x—is made by the accumulation in f up to a, plus the accumulation in f from a to x.
We knew when values of a function $r_f$ give the rate of change at every moment of a functionf, at each value in f’s domain there existed an interval of width ∆x containing that value that was small enough for which $r_f(x)$ was essentially constant.
Not knowing how wide these intervals were, we chose values of ∆x small enough so that our estimates were as accurate as we needed them to be.
We then introduced integral notation to represent the net accumulation $A_f(x)$ in the exact accumulation function from an initial value to any value of x.
In the next chapter we will address the second foundational problem
of calculus, namely:
You know how much of a quantity
there is at every moment; you want to know how fast it is varying at
every moment.