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Solutions Manual for Advanced Engineering Mathematics with MATLAB (5th Edition, 2022) by Duffy – Covers All Chapters

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INSTANT DOWNLOAD PDF — This solutions manual for Advanced Engineering Mathematics with MATLAB (5th Edition, 2022) by Dean G. Duffy provides complete, step-by-step solutions to textbook problems across a wide range of engineering mathematics topics. Subjects include differential equations, linear algebra, vector calculus, Laplace transforms, PDEs, and numerical methods, all supported with MATLAB implementation. Ideal for engineering students seeking to integrate theory with computation. engineering mathematics solutions manual, duffy 5th edition answers, matlab problem solving, differential equations with matlab, linear algebra exercises solved, pdes and laplace transform solutions, numerical methods engineering, advanced math textbook solutions, applied mathematics for engineers, matlab analytical solutions

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Uploaded on
July 5, 2025
Number of pages
596
Written in
2024/2025
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All Chapters Covered




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 = x dx, integra-
tion immediately gives −e−y = 21 x2 − C, or y = − ln(C − x2 /2).

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

3. Because the differential equation can be rewritten ln(x)dx/x = y dy, inte-
gration immediately gives 12 ln2 (x) + C = 21 y 2 , or y 2 (x) − ln2 (x) = 2C.

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

5. Because the differential equation can be rewritten y dy/(2+y 2 ) = x dx/(1+
x2 ), integration immediately gives 12 ln(2 + y 2 ) = 12 ln(1 + x2 ) + 21 ln(C), or
2 + y 2 (x) = C(1 + x2 ).

6. Because the differential equation can be rewritten dy/y 1/3 = x1/3 dx,
3/2
integration immediately gives 32 y 2/3 = 34 x4/3 + 32 C, or y(x) = 21 x4/3 + C .

1




@Seismicisolation
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, 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/(y 2 + 1) = (x3 +
5) dx, integration immediately gives tan−1 (y) = 14 x4 + 5x + C, or y(x) =
tan 14 x4 + 5x + C .

9. Because the differential equation can be rewritten y 2 dy/(b − ay 3 ) = 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(T0 − Γz)
Integrating from 0 to z,
     g/(RΓ)
p(z) g T0 − Γz p(z) T0 − Γz
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
 g/(RΓ)
T0 − ΓH
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
= − =− .
V + RV /S 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




@Seismicisolation
@Seismicisolation

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