Skip to main content
I believe this is corrects a minor typo
Source Link
Alwin
  • 5.1k
  • 11
  • 21

For a simple function like $x=t^2$ you can show that the chain rule works.

$x=t^2 \to \dot x = v = 2t \to \ddot x = \dot v = a = 2$

$x=t^{1/2} \to v=2x^{1/2} \to \frac{dv}{dx} = x^{-1/2}= 1/t$$t=x^{1/2} \to v=2x^{1/2} \to \frac{dv}{dx} = x^{-1/2}= 1/t$

$\frac {dv}{dx} \cdot v = 1/t \cdot 2t = 2 = a$

enter image description here

Looking at the slopes of the graphs you can imagine that as time progresses the increasing gradient of the one on the left multiplied by the decreasing gradient of the one in the middle could produce a constant value for the graph on the right.

For a simple function like $x=t^2$ you can show that the chain rule works.

$x=t^2 \to \dot x = v = 2t \to \ddot x = \dot v = a = 2$

$x=t^{1/2} \to v=2x^{1/2} \to \frac{dv}{dx} = x^{-1/2}= 1/t$

$\frac {dv}{dx} \cdot v = 1/t \cdot 2t = 2 = a$

enter image description here

Looking at the slopes of the graphs you can imagine that as time progresses the increasing gradient of the one on the left multiplied by the decreasing gradient of the one in the middle could produce a constant value for the graph on the right.

For a simple function like $x=t^2$ you can show that the chain rule works.

$x=t^2 \to \dot x = v = 2t \to \ddot x = \dot v = a = 2$

$t=x^{1/2} \to v=2x^{1/2} \to \frac{dv}{dx} = x^{-1/2}= 1/t$

$\frac {dv}{dx} \cdot v = 1/t \cdot 2t = 2 = a$

enter image description here

Looking at the slopes of the graphs you can imagine that as time progresses the increasing gradient of the one on the left multiplied by the decreasing gradient of the one in the middle could produce a constant value for the graph on the right.

Source Link
Farcher
  • 99.9k
  • 5
  • 83
  • 215

For a simple function like $x=t^2$ you can show that the chain rule works.

$x=t^2 \to \dot x = v = 2t \to \ddot x = \dot v = a = 2$

$x=t^{1/2} \to v=2x^{1/2} \to \frac{dv}{dx} = x^{-1/2}= 1/t$

$\frac {dv}{dx} \cdot v = 1/t \cdot 2t = 2 = a$

enter image description here

Looking at the slopes of the graphs you can imagine that as time progresses the increasing gradient of the one on the left multiplied by the decreasing gradient of the one in the middle could produce a constant value for the graph on the right.