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Solutions Manual for Advanced Engineering Mathematics with MATLAB (5th Edition) by Duffy – Complete Step-by-Step Solutions

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Instant PDF download after purchase. This complete solutions manual for Advanced Engineering Mathematics with MATLAB (5th Edition) by Duffy provides fully worked-out solutions to every chapter problem and exercise. It covers a wide range of topics including differential equations, linear algebra, complex analysis, vector calculus, numerical methods, transforms, and MATLAB applications. Each solution is clearly explained with detailed mathematical derivations and MATLAB code examples to support computational learning. Perfect for engineering, mathematics, and applied science students seeking clear guidance and verified answers for mastering advanced problem-solving with MATLAB.

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Institution
Advanced Engineering Mathematics
Course
Advanced Engineering Mathematics











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Institution
Advanced Engineering Mathematics
Course
Advanced Engineering Mathematics

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Uploaded on
October 27, 2025
Number of pages
602
Written in
2025/2026
Type
Exam (elaborations)
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SOLUTIONS

,Table of Contents
Chapter 1: First-Order Ordinary Differential Equations 1
Chapter 2: Higher-Order Ordinary Differential Equations
Chapter 3: Linear Algebra
Chapter 4: Vector Calculus
Chapter 5: Fourier Series
Chapter 6: The Fourier Transform
Chapter 7: The Laplace Transform
Chapter 8: The Wave Equation
Chapter 9: The Heat Equation
Chapter 10: Laplace’s Equation
Chapter 11: The Sturm-Liouville Problem
Chapter 12: Special Functions
Appendix A: Derivation of the Laplacian in Polar Coordinates
Appendix B: Derivation of the Laplacian in Spherical Polar Coordinates

, Solution Manual
Section 1.1

1. first-order, linear 2. first-order, nonlinear
3. first-order, nonlinear 4. third-order, linear
5. second-order, linear 6. first-order, nonlinear
7. third-order, nonlinear 8. second-order, linear
9. second-order, nonlinear 10. first-order, nonlinear
11. first-order, nonlinear 12. second-order, nonlinear
13. first-order, nonlinear 14. third-order, linear
15. second-order, nonlinear 16. third-order, nonlinear

Section 1.2

1. Because the differential equation can be rewritten e−y dy = xdx, integra-
tion immediately gives —e−y =2 1 x2 — C, or y = — ln(C — x2/2).

2. Separating variables, we have that dx/(1 + x2) = dy/(1 + y2). Integrating
— tan− (y) = tan(C), or (x
this equation, we find that tan−1(x) — y)/(1+xy) =
1

C.

3. Because the differential equation can be rewritten ln(x)dx/x = y dy, inte-
gration immediately gives2 1 ln2(x) + C = 21 y2, or y2(x) — ln2(x) = 2C.

4. Because the differential equation can be rewritten y2 dy = (x + x3) dx,
integration immediately gives y3(x)/3 = x2/2 + x4/4 + C.

5.2 Because the differential equation can1 be rewritten y dy/(2+y2) = xdx/(1+
x ), integration immediately gives ln(2 + y2) = 1 ln(1 + x2) + 1 ln(C), or
2 2 2
2 + y2(x) = C(1 + x2).

6. Because the differential equation can be rewritten dy/y1/3 = x1/3 dx,
3/2
integration immediately gives
2
y =4 3 x4/3 +2 3 C, or y(x) = 12 x4/3 + C
3 2/3
.

1

, 2 Advanced Engineering Mathematics with MATLAB

7. Because the differential equation can be rewritten e−y dy = ex dx, integra-
tion immediately gives —e−y = ex — C, or y(x) = — ln(C — ex).

8. Because the differential equation can be rewritten dy/(y2 + 1) = (x3 +
5) dx, integration immediately gives tan−1(y) = 1 x4 + 5x + C, or y(x) =
4
tan 41 x4 + 5x + C .

9. Because the differential equation can be rewritten y2 dy/(b — ay3) = dt,
y
integration immediately gives ln[b — ay 3] y0 = —3at, or (ay 3 — b)/(ay03 — b) =
e−3at.

10. Because the differential equation can be written du/u = dx/x2, integra-
tion immediately gives u = Ce−1/x or y(x) = x + Ce−1/x.

11. From the hydrostatic equation and ideal gas law, dp/p =— g dz/(RT ).
Substituting for T (z),
dp g
=— dz.
p R(T 0 — Γz)
Integrating from 0 to z,

p(z) g T0 — Γz p(z) T0 — Γz g/(RΓ)
ln = ln , or = .
p0 RΓ T0 p0 T0


12. For 0 < z < H, we simply use the previous problem. At z = H, the
pressure is
T0 — ΓH g/(RΓ)
p(H) = p0 .
T0
Then we follow the example in the text for an isothermal atmosphere for
z ≥ H.

13. Separating variables, we find that
dV dV R dV dt
2/S
= — =— .
V + RV V S(1 + RV/S) RC

Integration yields

V t
ln =— + ln(C).
1 + RV/S RC

Upon applying the initial conditions,

V0 RV0/S
V (t) = e−t/(RC) + e−t/(RC)V (t).
1 + RV0/S 1 + RV0/S

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