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Total differential

And there are never really endings, happy or otherwise. Things keep going on, they overlap and blur, your story is part of your sister’s story is part of many other stories, and there is no telling where any of them may lead. Everything turns in circles and spirals with the cosmic heart until infinity.

Recall

In particular, n = 2, this means that a critical point (x0, y0), $\frac{\partial f}{\partial x}(x_0, y_0) = 0$ and $\frac{\partial f}{\partial y}(x_0, y_0) = 0$

Total differential

Implicit differentiation is a technique used to find the derivative of functions defined implicitly, rather than explicitly or to find derivatives of functions that cannot be explicitly solved for one variable, y = f(x), dy = f’(x)dx, e.g., y = sin-1(x) ⇒ x = sin(y) ⇒ dx = cos(y)dy ⇒ $\frac{dy}{dx}=\frac{1}{cos(y)}$=[Using the Pythagorean identity cos(y) = $\sqrt{1-sin^2(y)}$ and since sin(y)=x] $\frac{1}{\sqrt{1-x^2}}$.

The total differential of a multivariable function w = f(x1, x2, ···,xn) describes how small changes in each of its variables affects the function’s value. It is denoted by df and is defined as follows: $\frac{df}{dt} =\frac{\partial f}{\partial x}d_x+\frac{\partial f}{\partial y}d_y+\frac{\partial f}{\partial z}d_z = f_xdx + f_ydy +f_zdz$ where $f_x = \frac{\partial f}{\partial x}, f_y = \frac{\partial f}{\partial y}$, and $f_z = \frac{\partial f}{\partial z}$ are the partial derivatives of f.

Using Different Notation

When considering how w changes with respect to another variable t, we can write: $\frac{dw}{dt} = w_x\frac{dx}{dt}+ w_y\frac{dy}{dt}+ w_z\frac{dz}{dt}$.

This can also be expressed using the gradient ∇w = ⟨wx, wy, wz⟩ and the derivate of the position vector $\vec{r}(t)$: $∇w·\frac{d\vec{r}}{dt}$, where $\frac{d\vec{r}}{dt} = ⟨\frac{dx}{dt}, \frac{dy}{dt}, \frac{dz}{dt}⟩$

The total differential tells us how the function w changes as you move along an infinitesimal displacement in each of its variables, hence providing information about the rate of change of the function in the x, y, and z directions. Besides, it provides a linear approximation of the function for small variations Δx, Δy, and Δz: Δw ≈ fxΔx + fyΔy + fzΔz.

The Chain Rule for multivariable functions

The Chain Rule for multivariable functions is a fundamental concept in calculus that allows us to compute the derivative of a composite function.

It states that if we have a function f(x, y, z) where x = x(t), y = y(t), and z = z(t) are functions of another variable t, then the derivate of f with respect to t is given by $\frac{df}{dt} = f_x\frac{dx}{dt} +f_y\frac{dy}{dt}+f_z\frac{dz}{dt}$.

Proof of the Chain Rule (2 versions)

Version 1: Using Total Differential

  1. Start with the total differential: df = $f_xdx + f_ydy +f_zdz,$ where x = x(t), y = y(t), and z = z(t) are functions of another variable t.
  2. Substitute dx = x’(t)dt, dy = y’(t), dz = z’(t)dt ⇒ df = $f_xdx + f_ydy +f_zdz = f_xx’(t)dt + f_yy’(t)dt +f_zz’(t)dt$.
  3. Divide by dt: $\frac{df}{dt} = f_x\frac{dx}{dt} +f_y\frac{dy}{dt}+f_z\frac{dz}{dt}.$

Version 2: Using Incremental Changes

  1. Approximate the change in f for small increments: Δf ≈ $f_xΔx + f_yΔy +f_zΔz$.
  2. Divide by Δt: $\frac{Δf}{Δt} = \frac{f_xΔx + f_yΔy +f_zΔz}{Δt} = f_x\frac{Δx}{Δt} + f_y\frac{Δy}{Δt} + f_z\frac{Δz}{Δt}⇒$.
  3. As Δt → 0, this approximation becomes exact and we get the Chain Rule again, $\frac{df}{dt} = f_x\frac{dx}{dt} +f_y\frac{dy}{dt}+f_z\frac{dz}{dt}.$

Exercises

$dz = \frac{∂z}{∂x}dx + \frac{∂z}{∂y}dy = 4xy^3dx + 6x^2y^2dy.$

$dz = \frac{∂z}{∂x}dx + \frac{∂z}{∂y}dy = e^xsin(y)dx + e^xcos(y)dy.$

f(2, 1) = 1·e2 ≈ 7.3891, f(2.5, 1.25) = 1·e2 = 1.25·e2.5 ≈ 15.2281. Δz = 15.2281-7.3891 = 7.839.

$Δz = \frac{∂z}{∂x}Δx + \frac{∂z}{∂y}Δy = ye^xΔx+ e^xΔy =$[Δx = 2.5 -2 = 0.5, Δy = 1.25 -1 = 0.25] = 1·e2·0.5 + e2·0.25 ≈ 5.5418. It is definitely not a good approximation.

Let’s apply the Chain Rule, $\frac{dw}{dt} = \frac{∂w}{∂x}\frac{dx}{dt} + \frac{∂w}{∂y}\frac{dy}{dt} + \frac{∂w}{∂z}\frac{dz}{dt} = 2xy·1 + x^2·e^t + 1·cos(t) =[\text{Since x = t and y =}e^t] 2te^t+t^2e^t+cos(t)$.

Alternatively, w(t) = x2y+z = t2et + sin(t) ⇒ $\frac{dw}{dt} = 2te^t+t^2e^t+cos(t)$. This confirms that both methods yield the same result.

We start with the total differential: $dw = f_xdx +f_ydy$ =[Since x and y are functions of u and v: $dx = \frac{∂x}{∂u}du + \frac{∂x}{∂v}dv = x_udu+x_vdv, dy = \frac{∂y}{∂u}du + \frac{∂y}{∂v}dv = y_udu+y_vdv$] $f_x(x_udu +x_vdv) +f_y(y_udu +y_vdv) = […]$

Collecting terms involving du and dv: = […] $(f_xx_u+f_yy_u)du + (f_xx_v + f_yy_v)dv$ ⇒ $\frac{\partial f}{\partial u} = f_xx_u+f_yy_u, \frac{\partial f}{\partial v} = f_xx_v + f_yy_v$.

Thus, we have, $\frac{\partial f}{\partial u} = \frac{\partial f}{\partial x}\frac{\partial x}{\partial u}+\frac{\partial f}{\partial y}\frac{\partial y}{\partial u}, \frac{\partial f}{\partial v} = \frac{\partial f}{\partial x}\frac{\partial x}{\partial v}+\frac{\partial f}{\partial y}\frac{\partial y}{\partial v}$.

We want to find: $\frac{\partial f}{\partial r} = \frac{\partial f}{\partial x}\frac{\partial x}{\partial r}+\frac{\partial f}{\partial y}\frac{\partial y}{\partial r} = f_xcos(θ) + f_ysin(θ)$

To approximate the change in temperature T given the changes in the head wind x, bird heart rate y, and flapping rate z, we can use the concept of the total differential in multivariable calculus.

Given the changes: Δx = 2m/s−1m/s = 1m/s, Δy = 55beats/min −50beats/min = 5beats/min, Δz = 4flaps/s −3flaps/s = 1flaps/s

Calculate the partial derivatives: $T_x = 0.18x + 1.4y, T_y = 1.4x, T_z = 190z.$

Calculate the total change in temperature:

$ΔT ≈ T_x(x, y, z)Δx + T_y(x, y, z)Δy + T_z(x, y, z)Δz =[\text{Substitute the given changes and values into the total differential}] (0.18x + 1.4y)Δx + 1.4xΔy + 190zΔz = (0.18·1 + 1.4·50)(2-1) + 1.4·1(55-50) + 190·3·1 = 70.18⋅1+1.4⋅5+570⋅1 ≈ 647.18$. Thus, the approximate change in temperature is 647.18 °C.

Bibliography

This content is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License and is based on MIT OpenCourseWare [18.01 Single Variable Calculus, Fall 2007].
  1. NPTEL-NOC IITM, Introduction to Galois Theory.
  2. Algebra, Second Edition, by Michael Artin.
  3. LibreTexts, Calculus and Calculus 3e (Apex). Abstract and Geometric Algebra, Abstract Algebra: Theory and Applications (Judson).
  4. Field and Galois Theory, by Patrick Morandi. Springer.
  5. Michael Penn, and MathMajor.
  6. Contemporary Abstract Algebra, Joseph, A. Gallian.
  7. YouTube’s Andrew Misseldine: Calculus. College Algebra and Abstract Algebra.
  8. MIT OpenCourseWare 18.01 Single Variable Calculus, Fall 2007 and 18.02 Multivariable Calculus, Fall 2007.
  9. Calculus Early Transcendentals: Differential & Multi-Variable Calculus for Social Sciences.
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