Recall:
$$ \rho c_p \left[ \frac{\partial T}{\partial t}+ (\vec v \cdot \vec \nabla) T \right] = k\vec\nabla^2T + \dot{S_v} $$
$$ T(0,t)=T_s $$
$$ q_s = -k\vec \nabla T $$
For 1-dimension:
$$ q_s = -k\frac{\partial T}{\partial x}\vert_{boundary} $$
$$ \frac{\partial T}{\partial x}\vert_{boundary} = 0 $$
$$ q = -k\frac{\partial T}{\partial x}\vert_{boundary}=h[T_\infty - T(0,t)] $$
<aside> 💡 Assumptions:
Recall Differential Form of Heat Transport Equation:
k\vec \nabla^2T + \cancel{\dot S_v} $$
First Term cancelled as Steady State
Second Term cancelled as NO Advection
Last Term cancelled as NO Heat Generation
$$ \therefore \frac{\partial^2T}{\partial x^2} = 0 \quad\to\quad T=C_1x+C_2 $$
Apply Boundary Conditions: $T = T_\text{s, 0}$ at $x=0$:
$$ C_2 = T_\text{s, 0} $$
$T=T_\text{s, L}$ at $x=L$:
$$ C_1 = \frac{T_\text{s, L} - T_\text{s, 0}}{L} $$
Therefore, the Temperature Profile is LINEAR:
$$ T = \frac{T_\text{s, L} - T_\text{s, 0}}{L}x + T_\text{s, 0} $$