Darcy's Law is given by the equation:
\[ Q = K \cdot A \cdot i \]
Where:
The given cross-sectional area is in square meters (m²). We need to convert it to square centimeters (cm²):
\[ A = 10 \, \text{m}^2 = 10 \times 10^4 \, \text{cm}^2 = 100000 \, \text{cm}^2 \]
Substitute the given values into Darcy's Law:
\[ Q = 0.25 \, \text{cm/s} \cdot 100000 \, \text{cm}^2 \cdot 0.04 \]
Now, calculate the volume of water flowing per second:
\[ Q = 1000 \, \text{cm}^3/\text{s} \]
The volume of water flowing per second is: 1000 cm³/s (rounded to three decimal places).
In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is _.
The units A to H marked on the figure represent different rock formations. Select the option that describes the chronological sequence from old to young.
Consider two intersecting, north-easterly striking and south-easterly dipping dikes Y1 and Y2, which are exposed on an east-west trending vertical wall of a granite (X) quarry as shown below.
The angle that the dikes make with the horizontal on the quarry wall is