The fractional compression \(\frac{\Delta V}{V}\) is given by:
\[ \frac{\Delta V}{V} = -\frac{\Delta P}{B} \]
The pressure \(\Delta P\) at the bottom of the ocean is:
\[ \Delta P = \rho gh = 1000 \times 10 \times 4000 = 4 \times 10^7 \, \text{Pa} \]
Thus,
\[ \frac{\Delta V}{V} = -\frac{4 \times 10^7}{2 \times 10^9} = -2 \times 10^{-2} \]
Therefore, \(\alpha = 2\).
The portion of the line \( 4x + 5y = 20 \) in the first quadrant is trisected by the lines \( L_1 \) and \( L_2 \) passing through the origin. The tangent of an angle between the lines \( L_1 \) and \( L_2 \) is: