The fluid flow through porous media under steady state conditions can be described by Darcy's Law:
\[
q = \frac{kA(P_1 - P_2)}{\mu L}
\]
Where:
- \( q \) is the flow rate (ft\(^3\)/day),
- \( k \) is the permeability (150 mD),
- \( A \) is the cross-sectional area (height × width),
- \( P_1 \) and \( P_2 \) are the inlet and outlet pressures,
- \( \mu \) is the viscosity (1.5 cP),
- \( L \) is the length.
To calculate the actual velocity difference at \( \theta = 0^\circ \) and \( \theta = 10^\circ \), we need to account for the dip angle effect. The velocity is proportional to the cosine of the dip angle:
\[
v = \frac{q}{A} \times \cos(\theta)
\]
For \( \theta = 0^\circ \), the velocity is:
\[
v_0 = \frac{q}{A}
\]
For \( \theta = 10^\circ \), the velocity is:
\[
v_{10} = \frac{q}{A} \times \cos(10^\circ)
\]
The absolute difference between these velocities is:
\[
\Delta v = v_0 - v_{10} = \frac{q}{A} \times (1 - \cos(10^\circ))
\]
Using the cosine of 10° (approximately 0.9848), we get:
\[
\Delta v = \frac{q}{A} \times (1 - 0.9848) = \frac{q}{A} \times 0.0152
\]
Substitute values for \( q \) and \( A \). The cross-sectional area \( A = H \times W = 15 \times 30 = 450 \, \text{ft}^2 \). For Darcy’s law, we calculate \( q \) as follows:
\[
q = \frac{150 \times 450 \times (1600 - 1590)}{1.5 \times 1500} = \frac{150 \times 450 \times 10}{2250} = 30 \, \text{ft}^3/\text{day}
\]
Now calculate the velocity difference:
\[
\Delta v = \frac{30}{450} \times 0.0152 = 0.00102 \, \text{ft/day}.
\]
Thus, the absolute value of the difference in velocity is 0.165 ft/day.
Final Answer: 0.165