The formula to calculate porosity (\(n\)) is given by:
\[ n = \frac{V_{\text{voids}}}{V_{\text{total}}} \times 100 \]
Where:
To calculate the volume of voids, we use the following equation:
\[ V_{\text{voids}} = V_{\text{total}} - V_{\text{solids}} \]
Given:
First, calculate the volume of solids:
\[ V_{\text{solids}} = \frac{\text{Mass of solids}}{\text{Particle density}} = \frac{1908 \, \text{g}}{2.65 \, \text{g/cc}} = 720 \, \text{cc} \]
Now, calculate the volume of voids:
\[ V_{\text{voids}} = 1200 \, \text{cc} - 720 \, \text{cc} = 480 \, \text{cc} \]
Now, we can calculate the porosity using the formula:
\[ n = \frac{480 \, \text{cc}}{1200 \, \text{cc}} \times 100 = 40\% \]
The porosity of the soil sample is: 40%.
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