To ascertain the fractional compression \( \frac{\Delta V}{V} \) of water at ocean depths, we apply the definition of the bulk modulus \( B \):
Bulk Modulus Relation:
\( B = -\frac{\Delta P}{\frac{\Delta V}{V}} \)
Where:
The pressure increase \( \Delta P \) at the ocean floor is calculated using hydrostatic pressure:
Hydrostatic Pressure Formula:
\( \Delta P = \rho g h \)
Where:
Substituting the given values yields:
\[ \Delta P = 1000 \times 10 \times 4000 = 4 \times 10^7 \, \text{N/m}^2 \]
Rearranging the bulk modulus equation to solve for fractional volume change:
\[ \frac{\Delta V}{V} = -\frac{\Delta P}{B} \]
Inserting the calculated \( \Delta P \) and provided \( B \) values:
\[ \frac{\Delta V}{V} = -\frac{4 \times 10^7}{2 \times 10^9} = -0.02 \]
Expressed in the format \( \alpha \times 10^{-2} \), this gives:
\[ \alpha = 2 \]
Confirmation:
The calculated \( \alpha = 2 \) aligns with the specified range of 2,2, validating the result.