The height of a mercury barometer is 75 cm at sea level and 50 cm at the top of a hill. Ratio of density of mercury to that of air is 10 4 . The height of the hill is
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Difference of pressure between sea level and the top of hill
Δ Δ P $= (h_1 - h_2) \times \rho_{\mathrm{Hg}} \times g = (75 - 50) \times 10^{-2} \times \rho_{\mathrm{Hg}} \times g$ …(i)
and pressure difference due to h meter of air
Δ Δ P = $h \times \rho_{air} \times g$ …(ii)
By equating (i) and (ii) we get
$h \times \rho_{\text{air}} \times g = (75 - 50) \times 10^{-2} \times \rho_{\text{Hg}} \times g$ $\therefore h = 25 \times 10^{-2} \left(\frac{\rho_{\text{Hg}}}{\rho_{\text{air}}}\right) = 25 \times 10^{-2} \times 10^{4} = 2500 \text{m}$
∴ ∴ Height of the hill = 2.5 km.
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