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conduction Fourier steady unsteady

Introduction to Heat Conduction

Heat conduction is one of the fundamental modes of heat transfer, alongside convection and radiation. It refers to the transfer of thermal energy within a material or between materials in direct physical contact, without any bulk movement of the material itself. Imagine holding one end of a metal rod while the other end is heated; over time, your hand feels warmth as heat travels through the rod. This transfer occurs due to the microscopic collisions and vibrations of particles within the solid.

Understanding conduction is essential in mechanical engineering because it governs how heat moves through machine components, insulation, and structural materials. Efficient thermal management ensures safety, performance, and energy savings in engineering systems.

Two key conduction scenarios are:

  • Steady State Conduction: When temperatures at every point in the material remain constant over time. For example, a wall with a constant temperature difference across it for a long time.
  • Unsteady (Transient) Conduction: When temperatures change with time, such as when a hot object cools down in air.

This section will explore the physical principles of conduction, introduce Fourier's law, and analyze both steady and unsteady conduction with practical engineering examples.

Fourier's Law of Heat Conduction

At the heart of conduction analysis lies Fourier's law, which quantifies the rate of heat transfer through a material due to a temperature gradient. It states that the heat flux (heat transfer per unit area per unit time) is proportional to the negative of the temperature gradient.

Mathematically, Fourier's law in one dimension is expressed as:

Fourier's Law of Heat Conduction

\[q = -k A \frac{dT}{dx}\]

Heat transfer rate through a solid due to conduction

q = Heat transfer rate (W)
k = Thermal conductivity (W/m·K)
A = Cross-sectional area (m²)
\(\frac{dT}{dx}\) = Temperature gradient (K/m)
Solid Slab Heat flow direction (q) T1 T2 Temperature gradient \(\frac{dT}{dx}\)

Here, k is a material property called thermal conductivity, which measures how well the material conducts heat. Metals like copper have high thermal conductivity, while insulators like wood have low values.

The negative sign indicates heat flows from higher to lower temperature regions, consistent with natural heat flow direction.

Steady State One-Dimensional Conduction

In many engineering problems, heat conduction reaches a steady state where temperatures no longer change with time. This simplifies analysis since the temperature distribution depends only on position.

Consider a plane wall of thickness \(L\), cross-sectional area \(A\), with one side at temperature \(T_1\) and the other at \(T_2\). Assuming constant thermal conductivity and no internal heat generation, the temperature varies linearly across the wall.

Plane Wall T1 T2 Linear Temperature Gradient

The temperature distribution \(T(x)\) is given by:

Temperature Distribution in Plane Wall

\[T(x) = T_1 - \frac{(T_1 - T_2)}{L} x\]

Linear variation of temperature across thickness

x = Distance from hot side (m)

The heat transfer rate through the wall is constant and calculated as:

Steady State Heat Transfer Through Plane Wall

\[q = \frac{k A (T_1 - T_2)}{L}\]

Heat transfer rate through a plane wall

q = Heat transfer rate (W)
k = Thermal conductivity (W/m·K)
A = Cross-sectional area (m²)
L = Thickness of wall (m)

This formula is widely used in building insulation, heat exchanger walls, and machine components.

Thermal Resistance and Composite Walls

Often, heat must pass through multiple layers of different materials, such as brick walls with insulation or pipes with coatings. To analyze such composite walls, we use the concept of thermal resistance, analogous to electrical resistance in circuits.

Each layer offers resistance to heat flow, calculated as:

Thermal Resistance for Conduction

\[R_{cond} = \frac{L}{k A}\]

Resistance offered by a solid layer to heat conduction

\(R_{cond}\) = Thermal resistance (K/W)
L = Thickness (m)
k = Thermal conductivity (W/m·K)
A = Cross-sectional area (m²)

For layers in series, total resistance is the sum of individual resistances:

Total Thermal Resistance in Series

\[R_{total} = \sum R_i = \sum \frac{L_i}{k_i A}\]

Sum of resistances for multiple layers

\(R_i\) = Thermal resistance of i-th layer (K/W)

Heat transfer rate through the composite wall is then:

Heat Transfer Through Composite Wall

\[q = \frac{T_1 - T_n}{R_{total}}\]

Heat transfer rate through multiple layers

\(T_1, T_n\) = Temperatures at boundaries (K)
Layer Thickness \(L_i\) (m) Thermal Conductivity \(k_i\) (W/m·K) Area \(A\) (m²) Thermal Resistance \(R_i = \frac{L_i}{k_i A}\) (K/W)
Brick 0.2 0.72 10 0.0278
Insulation 0.05 0.04 10 0.125

This analogy simplifies complex conduction problems into manageable calculations.

Unsteady State Conduction - Lumped System Analysis

When temperatures vary with time, conduction becomes unsteady or transient. Exact solutions can be complex, but a useful simplification is the lumped capacitance method, which assumes the entire body has a uniform temperature at any instant.

This assumption holds when internal temperature gradients are negligible compared to surface temperature differences. The criterion for this is the Biot number (\(Bi\)):

Biot Number

\[Bi = \frac{h L_c}{k}\]

Dimensionless number to check lumped system validity

h = Convective heat transfer coefficient (W/m²·K)
\(L_c\) = Characteristic length (m)
k = Thermal conductivity (W/m·K)

If \(Bi < 0.1\), lumped capacitance method is valid.

graph TD    A[Start: Given problem] --> B{Calculate Biot number \(Bi = \frac{h L_c}{k}\)}    B -->|Bi < 0.1| C[Use Lumped Capacitance Method]    B -->|Bi ≥ 0.1| D[Use Analytical or Numerical Methods]    C --> E[Apply temperature variation formula]    D --> F[Refer to Heisler charts or solve transient conduction equations]

Temperature variation with time is given by:

Lumped Capacitance Method

\[\frac{T - T_\infty}{T_i - T_\infty} = e^{-\frac{h A}{\rho c_p V} t}\]

Temperature variation of a body cooling/heating in fluid

T = Temperature at time t (K)
\(T_\infty\) = Ambient temperature (K)
\(T_i\) = Initial temperature (K)
h = Convective heat transfer coefficient (W/m²·K)
A = Surface area (m²)
\(\rho\) = Density (kg/m³)
\(c_p\) = Specific heat (J/kg·K)
V = Volume (m³)
t = Time (s)

Unsteady State Conduction - Analytical Solutions and Heisler Charts

For cases where \(Bi > 0.1\), temperature gradients inside the body cannot be ignored. Analytical solutions of transient conduction equations become necessary but are mathematically involved.

One common scenario is transient conduction in a semi-infinite solid, where heat penetrates gradually over time. The temperature at depth \(x\) and time \(t\) is given by solutions involving error functions.

To simplify exam calculations, engineers use Heisler charts, graphical tools that provide temperature distributions and heat transfer rates for standard geometries like slabs, cylinders, and spheres under transient conditions.

Surface (x=0) Depth (x increases) Temperature Profile at time t

Heisler charts allow quick estimation of transient temperatures without solving complex equations, a valuable skill for competitive exams.

Formula Bank

Formula Bank

Fourier's Law of Heat Conduction
\[ q = -k A \frac{dT}{dx} \]
where: \(q\) = heat transfer rate (W), \(k\) = thermal conductivity (W/m·K), \(A\) = cross-sectional area (m²), \(\frac{dT}{dx}\) = temperature gradient (K/m)
Steady State Heat Transfer Through Plane Wall
\[ q = \frac{k A (T_1 - T_2)}{L} \]
where: \(q\) = heat transfer rate (W), \(k\) = thermal conductivity (W/m·K), \(A\) = area (m²), \(T_1, T_2\) = temperatures on either side (K), \(L\) = thickness (m)
Thermal Resistance for Conduction
\[ R_{cond} = \frac{L}{k A} \]
where: \(R_{cond}\) = thermal resistance (K/W), \(L\) = thickness (m), \(k\) = thermal conductivity (W/m·K), \(A\) = area (m²)
Overall Heat Transfer Rate Through Composite Wall
\[ q = \frac{T_1 - T_n}{\sum R_i} \]
where: \(q\) = heat transfer rate (W), \(T_1, T_n\) = temperatures at boundaries (K), \(R_i\) = thermal resistance of each layer (K/W)
Lumped Capacitance Method
\[ \frac{T - T_\infty}{T_i - T_\infty} = e^{-\frac{h A}{\rho c_p V} t} \]
where: \(T\) = temperature at time \(t\) (K), \(T_\infty\) = ambient temperature (K), \(T_i\) = initial temperature (K), \(h\) = convective heat transfer coefficient (W/m²·K), \(A\) = surface area (m²), \(\rho\) = density (kg/m³), \(c_p\) = specific heat (J/kg·K), \(V\) = volume (m³), \(t\) = time (s)
Biot Number
\[ Bi = \frac{h L_c}{k} \]
where: \(Bi\) = Biot number (dimensionless), \(h\) = convective heat transfer coefficient (W/m²·K), \(L_c\) = characteristic length (m), \(k\) = thermal conductivity (W/m·K)
Example 1: Heat Transfer Through a Composite Wall Medium
A wall consists of two layers: 0.2 m thick brick (\(k = 0.72\) W/m·K) and 0.05 m thick insulation (\(k = 0.04\) W/m·K). The wall area is 10 m². The inside surface temperature is 30°C and outside surface temperature is 5°C. Calculate the heat loss through the wall.

Step 1: Calculate thermal resistance of each layer using \(R = \frac{L}{k A}\).

Brick resistance: \(R_1 = \frac{0.2}{0.72 \times 10} = 0.0278\) K/W

Insulation resistance: \(R_2 = \frac{0.05}{0.04 \times 10} = 0.125\) K/W

Step 2: Calculate total resistance:

\(R_{total} = R_1 + R_2 = 0.0278 + 0.125 = 0.1528\) K/W

Step 3: Calculate heat loss:

\(q = \frac{T_1 - T_2}{R_{total}} = \frac{30 - 5}{0.1528} = \frac{25}{0.1528} = 163.7\) W

Answer: Heat loss through the wall is approximately 164 W.

Example 2: Cooling of a Hot Metal Sphere Using Lumped Capacitance Medium
A metal sphere of diameter 0.1 m initially at 150°C is suddenly exposed to air at 30°C with convective heat transfer coefficient \(h = 25\) W/m²·K. The sphere has density \(\rho = 7800\) kg/m³, specific heat \(c_p = 460\) J/kg·K, and thermal conductivity \(k = 45\) W/m·K. Calculate the temperature of the sphere after 10 minutes. Check if lumped capacitance method is applicable.

Step 1: Calculate characteristic length \(L_c = \frac{V}{A}\).

Volume \(V = \frac{4}{3} \pi r^3 = \frac{4}{3} \pi (0.05)^3 = 5.24 \times 10^{-4}\) m³

Surface area \(A = 4 \pi r^2 = 4 \pi (0.05)^2 = 0.0314\) m²

So, \(L_c = \frac{5.24 \times 10^{-4}}{0.0314} = 0.0167\) m

Step 2: Calculate Biot number \(Bi = \frac{h L_c}{k} = \frac{25 \times 0.0167}{45} = 0.0093 < 0.1\).

Lumped capacitance method is valid.

Step 3: Calculate temperature after time \(t = 600\) s using:

\[ \frac{T - T_\infty}{T_i - T_\infty} = e^{-\frac{h A}{\rho c_p V} t} \]

Calculate exponent:

\[ \frac{h A}{\rho c_p V} = \frac{25 \times 0.0314}{7800 \times 460 \times 5.24 \times 10^{-4}} = \frac{0.785}{1880} = 0.000417 \text{ s}^{-1} \]

Exponent value: \(0.000417 \times 600 = 0.250\)

Calculate temperature ratio:

\[ \frac{T - 30}{150 - 30} = e^{-0.25} = 0.7788 \]

Calculate \(T\):

\(T = 30 + 0.7788 \times 120 = 30 + 93.46 = 123.46^\circ C\)

Answer: Temperature of the sphere after 10 minutes is approximately 123.5°C.

Example 3: Steady State Heat Conduction Through a Plane Wall Easy
A steel plate 10 mm thick and 0.5 m² in area has temperatures of 100°C and 40°C on its two faces. Thermal conductivity of steel is 45 W/m·K. Find the heat transfer rate through the plate.

Step 1: Convert thickness to meters: 10 mm = 0.01 m.

Step 2: Use steady state heat conduction formula:

\[ q = \frac{k A (T_1 - T_2)}{L} = \frac{45 \times 0.5 \times (100 - 40)}{0.01} = \frac{45 \times 0.5 \times 60}{0.01} \]

\[ q = \frac{1350}{0.01} = 135000 \text{ W} \]

Answer: Heat transfer rate is 135 kW.

Example 4: Use of Heisler Chart for Transient Heat Conduction Hard
A large steel slab 0.1 m thick is initially at 200°C. It is suddenly exposed to air at 25°C with convective heat transfer coefficient \(h = 50\) W/m²·K. Calculate the temperature at the center of the slab after 5 minutes. Thermal conductivity \(k = 45\) W/m·K, density \(\rho = 7800\) kg/m³, specific heat \(c_p = 460\) J/kg·K.

Step 1: Calculate Biot number:

\[ Bi = \frac{h L_c}{k} = \frac{50 \times (0.1/2)}{45} = \frac{50 \times 0.05}{45} = 0.0556 < 0.1 \]

Since \(Bi < 0.1\), lumped capacitance method could be used, but for practice, we use Heisler chart.

Step 2: Calculate Fourier number:

\[ Fo = \frac{\alpha t}{L^2} \]

Thermal diffusivity \(\alpha = \frac{k}{\rho c_p} = \frac{45}{7800 \times 460} = 1.25 \times 10^{-5} \text{ m}^2/\text{s}\)

Time \(t = 5 \times 60 = 300\) s, thickness \(L = 0.1\) m

\[ Fo = \frac{1.25 \times 10^{-5} \times 300}{(0.1)^2} = \frac{3.75 \times 10^{-3}}{0.01} = 0.375 \]

Step 3: Using Heisler chart for slab at center, find dimensionless temperature ratio \(\theta/\theta_i\) for \(Bi=0.0556\) and \(Fo=0.375\). From charts, approximate \(\theta/\theta_i \approx 0.5\).

Step 4: Calculate temperature at center:

\[ \frac{T - T_\infty}{T_i - T_\infty} = 0.5 \implies T = T_\infty + 0.5 (T_i - T_\infty) = 25 + 0.5 (200 - 25) = 25 + 87.5 = 112.5^\circ C \]

Answer: Temperature at the center after 5 minutes is approximately 112.5°C.

Example 5: Heat Loss from a Pipe with Insulation Hard
A steel pipe of outer diameter 0.1 m is insulated with a 0.05 m thick layer of insulation. The pipe surface temperature is 150°C, and ambient air temperature is 30°C with convective heat transfer coefficient \(h = 20\) W/m²·K. Thermal conductivity of insulation is 0.04 W/m·K. Calculate the heat loss per meter length of the pipe.

Step 1: Calculate thermal resistances:

Pipe surface radius \(r_1 = 0.05\) m, insulation outer radius \(r_2 = 0.05 + 0.05 = 0.10\) m

Area for convection \(A_{conv} = 2 \pi r_2 \times 1 = 2 \pi \times 0.10 \times 1 = 0.628\) m²

Convection resistance:

\[ R_{conv} = \frac{1}{h A_{conv}} = \frac{1}{20 \times 0.628} = 0.0796 \text{ K/W} \]

Conduction resistance through insulation (cylindrical):

\[ R_{cond} = \frac{\ln(r_2/r_1)}{2 \pi k L} = \frac{\ln(0.10/0.05)}{2 \pi \times 0.04 \times 1} = \frac{0.693}{0.251} = 2.76 \text{ K/W} \]

Step 2: Total thermal resistance:

\[ R_{total} = R_{cond} + R_{conv} = 2.76 + 0.0796 = 2.8396 \text{ K/W} \]

Step 3: Calculate heat loss:

\[ q = \frac{T_s - T_\infty}{R_{total}} = \frac{150 - 30}{2.8396} = \frac{120}{2.8396} = 42.25 \text{ W/m} \]

Answer: Heat loss from the insulated pipe is approximately 42.3 W per meter length.

Tips & Tricks

Tip: Always calculate the Biot number before applying lumped capacitance method.

When to use: To quickly decide if lumped system analysis is valid for transient conduction problems.

Tip: Use thermal resistance analogy to simplify composite wall problems.

When to use: When dealing with multiple layers in series or parallel for steady state conduction.

Tip: Remember that steady state conduction temperature profile is linear in one dimension.

When to use: To quickly sketch or estimate temperature distribution in steady conduction.

Tip: Use Heisler charts for complex transient conduction problems to avoid lengthy calculations.

When to use: When analytical solutions are difficult and Biot number > 0.1.

Tip: Convert all units to SI (metric) before calculations to avoid errors.

When to use: Always, especially in competitive exams with mixed unit inputs.

Common Mistakes to Avoid

❌ Applying lumped capacitance method when Biot number > 0.1
✓ Calculate Biot number first; if > 0.1, use analytical or numerical methods instead
Why: Lumped system assumes negligible internal temperature gradients, invalid for large Biot numbers
❌ Confusing steady state with unsteady conduction conditions
✓ Identify problem conditions carefully; steady state assumes no temperature change with time
Why: Misinterpretation leads to wrong formula application and incorrect results
❌ Ignoring area changes in composite walls or cylindrical geometries
✓ Account for varying cross-sectional area or use appropriate formulas for cylindrical/radial conduction
Why: Heat transfer rate depends on actual conduction path area
❌ Mixing units, especially thickness in cm or mm with conductivity in W/m·K
✓ Convert all lengths to meters before calculations
Why: Unit inconsistency causes large errors in heat transfer rate
❌ Using steady state formulas for transient conduction problems
✓ Check problem statement and time dependency; use transient conduction methods if temperature varies with time
Why: Steady state assumes equilibrium, invalid for transient scenarios
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