Final Answer:
The temperature at a depth of 0.005 m from the highway surface after 125 minutes is approximately 45.7°C.
Step-by-step explanation:
To determine the temperature distribution within the asphalt, we can use the one-dimensional heat conduction equation:
![\[ \frac{{\partial T}}{{\partial t}} = \alpha \frac{{\partial^2 T}}{{\partial x^2}} \]](https://img.qammunity.org/2024/formulas/engineering/college/thylkc3qz6bve0wjg49iw30qa3ci7g0frz.png)
where (T) is the temperature, (t) is time, (x) is the depth, and
is the thermal diffusivity given by
.
In this case, the initial condition is (T(x, 0) = 55°C) and the boundary condition is (T(0, t) = 25°C ) (constant highway surface temperature after rain). We can solve this partial differential equation to find the temperature distribution with respect to depth and time.
After solving, the solution is:
![\[ T(x, t) = T_0 + \Delta T \cdot \text{{erfc}}\left(\frac{x}{{2 √(\alpha t)}}\right) \]](https://img.qammunity.org/2024/formulas/engineering/college/977si24u44h8m0cruybw2e0qh3m6bqziqv.png)
where
is the initial temperature,
is the temperature difference, and
is the complementary error function.
Plugging in the values, we get:
![\[ T(0.005, 125 * 60) \approx 45.7°C]](https://img.qammunity.org/2024/formulas/engineering/college/noknlc8jgns0jh84girav2z8hdg2869wwe.png)
This result indicates that after 125 minutes, the temperature at a depth of 0.005 m has stabilized at approximately 45.7°C, showing the gradual dissipation of heat through the asphalt.