1D Transient Heat Conduction Simulator Back
Thermal Analysis

1D Transient Heat Conduction Simulator — Initial-Boundary Problem (Explicit Scheme)

Finite difference simulation of 1D transient heat conduction. Change initial and boundary conditions to experience temperature profile evolution in real time.

Material & Parameters

Initial Condition

Boundary Conditions

Governing equation: $\dfrac{\partial T}{\partial t}= \alpha \dfrac{\partial^2 T}{\partial x^2}$
Explicit FD: $T_i^{n+1}= T_i^n + Fo(T_{i+1}^n - 2T_i^n + T_{i-1}^n)$
Stability: $Fo = \alpha\Delta t/\Delta x^2 \leq 0.5$
Results
Center T_mid
Max T_max
Time t
0 s
Fourier No. Fo
Diffusivity α
Left T
Right T
Convection h
Grid: 80 nodes Δt: s Domain L: 1.0 m
Temperature Profile T(x, t)
Center Temperature Transient T_mid(t)
Transient
Theory & Key Formulas

$$q = -k \frac{dT}{dx}$$

フーリエの熱伝導法則:熱流束 $q$(W/m²)は温度勾配に熱伝導率 $k$(W/mK)を掛けた値。

$$\frac{\partial T}{\partial t} = \alpha \frac{\partial^2 T}{\partial x^2}$$

1次元熱拡散方程式:$\alpha = k/(\rho c_p)$ は熱拡散率(m²/s)。

$$T(x,\infty) = T_L + \frac{T_R - T_L}{L}x$$

定常解析解:定常状態では温度は線形分布(境界条件が一定の場合)。

What is 1D Transient Heat Conduction?

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What exactly is "transient" heat conduction? How is it different from the steady-state heat flow I learned about before?
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Great question! "Steady-state" means temperatures have stopped changing over time—like a hot coffee mug that's finally cooled to room temperature. "Transient" is the exciting part before that, where temperatures are actively evolving. In this simulator, you're watching that evolution happen in real-time. Try changing the "Material Preset" from copper to glass wool and see how much slower the temperature profile changes.
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Wait, really? So the material itself changes how fast heat moves? What's the physical property that controls that speed?
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Exactly! That key property is called thermal diffusivity, denoted by $\alpha$. It's a material's "thermal agility"—how quickly it can conduct heat relative to its ability to store thermal energy. A high $\alpha$, like copper's (~$1.2 \times 10^{-4}$ m²/s), means heat races through. A low $\alpha$, like glass wool's (~$4 \times 10^{-7}$ m²/s), means it's a great insulator. The simulator calculates this internally based on your material choice.
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Okay, I see the material matters. But what about the "Left BC" and "Right BC" sliders? What happens if I set one side to a fixed temperature and the other to be insulated?
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That's a perfect experiment! The "BC" stands for Boundary Condition—it's the rule you impose at the edges of your 1D rod. A fixed temperature (Dirichlet condition) forces that end to stay at a set value. An insulated condition (Neumann, with zero heat flux) means no heat can enter or escape that end. Try it: set a hot initial profile, fix the left side cold, and insulate the right. You'll see heat drain out the left while the right end's temperature gets "trapped" and changes very slowly.

Physical Model & Key Equations

The core physics is governed by the 1D Heat Diffusion Equation (Fourier's Law). It states that the rate of temperature change at any point is proportional to the spatial curvature (second derivative) of the temperature field.

$$ \frac{\partial T}{\partial t}= \alpha \frac{\partial^2 T}{\partial x^2}$$

Here, $T(x,t)$ is temperature, $t$ is time, $x$ is position, and $\alpha$ is the thermal diffusivity ($\alpha = \lambda / (\rho c_p)$). This equation is solved numerically in the simulator using the Finite Difference Method.

The numerical solution's stability is controlled by the Fourier Number, a dimensionless quantity. The simulator must keep this below a critical value for accurate, stable results.

$$ Fo = \frac{\alpha \Delta t}{\Delta x^2} \leq 0.5 $$

$Fo$ is the Fourier number, $\Delta t$ is the computational time step, and $\Delta x$ is the spatial grid size. This condition ensures the explicit numerical scheme doesn't produce unrealistic, oscillating results. The simulator automatically chooses a $\Delta t$ that satisfies this.

Frequently Asked Questions

If the time step Δt is too large, the numerical stability condition (CFL condition) of the finite difference method is not satisfied, causing divergence. Reduce Δt or increase the spatial step Δx so that αΔt/(Δx)^2 is approximately ≤ 0.5.
The initial condition is the temperature distribution of the entire rod at time 0 seconds (e.g., uniform 20°C). The boundary condition specifies the heat transfer at both ends of the rod. You can choose from fixed temperature (e.g., left end 100°C), adiabatic, convection, etc. It is easier to understand the behavior if you first try a simple fixed temperature.
The larger α is, the faster heat propagates. For example, copper (α ≈ 1.1×10⁻⁴ m²/s) spreads temperature changes rapidly, while wood (α ≈ 1×10⁻⁷ m²/s) does so very slowly. If α is increased by a factor of 10, the distance heat reaches in the same time becomes about 3 times larger.
The heat transfer coefficient h [W/m²K] represents the ease of heat transfer between the object surface and the surrounding fluid. Typical values are: 5–25 for still air, 10–100 for forced convection (e.g., a fan), and 100–1000 for water. A larger value causes the surface temperature to approach the ambient temperature more quickly.

Real-World Applications

Building Insulation Design: Engineers use this exact 1D analysis to model heat transfer through walls. By simulating transient conditions (like a hot day turning into a cool night), they can select the right insulation material (low $\alpha$) and thickness to maintain comfortable indoor temperatures and reduce energy costs.

Electronic Cooling: When a computer chip powers on, it generates heat in a pulse. Transient thermal analysis predicts how quickly that heat will diffuse through the chip package and into the heat sink. This prevents overheating and ensures reliable performance during sudden computational loads.

Food Processing & Safety: In canning or pasteurization, it's critical to ensure the coldest point inside the food reaches a sufficient temperature for a specific time to kill bacteria. 1D transient models help determine the required processing time for different food geometries and materials.

Geothermal Energy Systems: The design of ground-source heat pumps relies on understanding how heat extracted from (or injected into) the ground diffuses through the soil over days and seasons. Transient models inform the spacing and depth of underground piping loops for efficient, sustainable heating and cooling.

Common Misconceptions and Points to Note

First, do not confuse "thermal diffusivity" with "thermal conductivity". The "thermal diffusivity α" you directly adjust in the simulator determines the "speed" of temperature change. On the other hand, the "thermal conductivity λ" that appears on the backside in convection conditions is the very "ease of heat flow" itself. For example, glass wool insulation has a very small thermal conductivity (it does not conduct heat well), which consequently results in a small thermal diffusivity and a slow temperature change. If you don't understand this difference, you will be confused when looking at material data sheets to set parameters.

Next, the value of the heat transfer coefficient h in "convection" conditions is critical. It's fine to play with the default values, but to use this for practical work, investigating appropriate values is essential. For instance, the order of magnitude is completely different: for natural convection (air) it's about 5–25 W/(m²·K), for forced convection (air by fan) 25–250 W/(m²·K), and for water cooling 500–10000 W/(m²·K). If you uniformly set this to "let's say 100," you will get results far removed from reality.

Finally, always be mindful of the limitations of the 1D model. This tool is optimal for analyzing the "thickness direction" of rods or thick plates, but in reality, heat spreads three-dimensionally. For example, heat generated by a chip on a smartphone substrate also spreads within the plane of the substrate (2D). Keep in mind that the 1D model is a "first approximation" for understanding the "primary heat flow path" or the "representative behavior in a cross-section."

How to Use

  1. Enter thermal diffusivity (alpha) in m²/s—for copper use 1.17e-4, for concrete use 8.3e-7
  2. Set left boundary condition: fixed temperature (TL in °C) or convection coefficient (hConv in W/m²K)
  3. Set right boundary condition temperature (TR in °C)
  4. Adjust spatial grid and time step; simulator enforces Courant criterion Fo = alpha·dt/dx² ≤ 0.5 for stability
  5. Click Simulate to compute temperature field evolution over domain length

Worked Example

Steel rod (alpha = 1.2e-5 m²/s, length 0.1 m) with TL = 100°C fixed, TR = 20°C fixed, initial uniform 20°C. Using dx = 0.01 m and dt = 5 s gives Fo = 0.06. After 300 s, midpoint temperature rises to approximately 58°C. Increasing hConv to 50 W/m²K at left boundary (ambient 100°C) produces slower interior heating due to convective resistance.

Practical Notes

  1. Stability failure appears as oscillating or divergent temperatures—reduce dt or increase dx immediately
  2. For insulated boundary, set hConv = 0 W/m²K; for high convection cooling (e.g., quenching), use hConv > 500 W/m²K
  3. Coarse meshes (dx > 5 mm) miss local gradients; use at least 10 nodes across critical zones
  4. Transient duration scales as L²/alpha: thin films (1 mm aluminum) equilibrate in seconds; thick concrete (0.5 m) requires hours