Step 1: Understanding the Concept:
This problem involves an unsteady, compressible, one-dimensional fluid flow. The governing principle is the conservation of mass, which is expressed by the continuity equation in its differential form. The density is "spatially homogeneous," meaning it does not vary with position (\(x, y, z\)), only with time (\(t\)).
Step 2: Key Formula or Approach:
The Continuity Equation in its general form is:
\[ \frac{\partial \rho}{\partial t} + \nabla \cdot (\rho \vec{V}) = 0 \]
For a one-dimensional flow \(\vec{V} = u(x, t) \hat{i}\), this simplifies to:
\[ \frac{\partial \rho}{\partial t} + \frac{\partial(\rho u)}{\partial x} = 0 \]
Step 3: Detailed Explanation or Calculation:
Given data:
Velocity field, \(\vec{V} = u(x, t) \hat{i}\)
Density field, \(\rho(t) = 1 + 0.2e^{-t}\)
Boundary condition, \(u(0, t) = 1\)
Let's expand the continuity equation:
\[ \frac{\partial \rho}{\partial t} + \rho \frac{\partial u}{\partial x} + u \frac{\partial \rho}{\partial x} = 0 \]
Since the density \(\rho\) is only a function of time \(t\), its partial derivative with respect to space \(x\) is zero: \( \frac{\partial \rho}{\partial x} = 0 \).
The equation simplifies to:
\[ \frac{d \rho}{d t} + \rho \frac{\partial u}{\partial x} = 0 \]
First, find the time derivative of density, \(\frac{d\rho}{dt}\):
\[ \frac{d\rho}{dt} = \frac{d}{dt}(1 + 0.2e^{-t}) = -0.2e^{-t} \]
Substitute this and the expression for \(\rho(t)\) into the simplified continuity equation:
\[ -0.2e^{-t} + (1 + 0.2e^{-t}) \frac{\partial u}{\partial x} = 0 \]
Now, solve for the spatial gradient of velocity, \(\frac{\partial u}{\partial x}\):
\[ \frac{\partial u}{\partial x} = \frac{0.2e^{-t}}{1 + 0.2e^{-t}} \]
To find \(u(x, t)\), we need to integrate this expression with respect to \(x\). Since the right-hand side is only a function of \(t\), the integration is straightforward:
\[ u(x, t) = \int \left( \frac{0.2e^{-t}}{1 + 0.2e^{-t}} \right) dx = \left( \frac{0.2e^{-t}}{1 + 0.2e^{-t}} \right) x + f(t) \]
where \(f(t)\) is an arbitrary function of time that acts as the constant of integration.
We use the boundary condition \(u(0, t) = 1\) to find \(f(t)\):
\[ u(0, t) = \left( \frac{0.2e^{-t}}{1 + 0.2e^{-t}} \right) (0) + f(t) = 1 \]
This implies \(f(t) = 1\).
So, the complete velocity function is:
\[ u(x, t) = \frac{0.2e^{-t}}{1 + 0.2e^{-t}} x + 1 \]
Finally, we need to find the value of \(u(2, 1)\). Substitute \(x=2\) and \(t=1\):
\[ u(2, 1) = \left( \frac{0.2e^{-1}}{1 + 0.2e^{-1}} \right) (2) + 1 \]
Using the value \(e^{-1} \approx 0.36788\):
\[ u(2, 1) = \left( \frac{0.2 \times 0.36788}{1 + 0.2 \times 0.36788} \right) (2) + 1 \]
\[ u(2, 1) = \left( \frac{0.073576}{1 + 0.073576} \right) (2) + 1 = \left( \frac{0.073576}{1.073576} \right) (2) + 1 \]
\[ u(2, 1) \approx (0.06853) \times 2 + 1 = 0.13706 + 1 = 1.13706 \]
Step 4: Final Answer:
Rounding off to two decimal places, the value of u(2, 1) is 1.14.
Step 5: Why This is Correct:
The solution is derived directly from the fundamental principle of mass conservation (the continuity equation). The given conditions (unidirectional flow, spatially homogeneous density) were used to simplify the general equation. The integration and application of the boundary condition were performed correctly to find the explicit form of the velocity function. The final numerical evaluation yields a result of 1.14, which falls within the specified answer range of 1.10 to 1.20.