Initial conditions describe the state of the system at the beginning of observation, essentially providing the starting point for analyzing changes over time. In the context of heat conduction, it refers to the initial temperature distribution across the spatial domain of interest.
Before solving the heat equation for our circular plate, we need to know the temperature at every point \( (x, y) \) at \( t=0 \). For this exercise, there are four different initial conditions given:
- Condition (a): \( f(x,y) = \frac{T_{0}}{a} y \)
- Condition (b): \( f(x,y) = \frac{T_{0}}{a} x \)
- Condition (c): \( f(x,y) = \frac{T_{0}}{a^2} x y \)
- Condition (d): \( f(x,y) = T_{0} \)
Each condition lists a unique function that describes how temperature is distributed initially; some conditions change linearly with distance, while others remain uniform.
Using these initial conditions with the appropriate boundary conditions enables solving the heat equation effectively, defining how the temperature will change and spread within the plate over time. Importantly, the initial conditions dictate the initial direction and rate at which heat will progress through the plate.