An air bubble of radius 2.0 mm is formed at the bottom of a 3.3 m deep river. Calculate the radius of the bubble as it comes to the surface. Atmospheric pressure =1.0×105 Pa and density of water =1000 kg m−3
The pressure at a depth h = 3.3 m under water will be -
P=P0+ρgh (symbols have their usual meaning)
=105+1000×10×3.3 (P0=105 Pa; ρwater=1000 kg m−3;g=10 ms−2)
=1.33×105 Pa.
For simplicity we have to assume that gases inside the bubble don't get dissolved in the water as the bubble rises up. So, the number of moles stays fixed. It is also safe to assume constant temperature.
Volume of the bubble at the bottom of the river = [(43)×π×(2.0)3]mm3.
Let the radius of the bubble when it reaches the top be rmm , and volume (43)πr3mm3 denoted by V.
Since PV = nRT, if n and T are fixed, the product PV will be a constant.
∴(1.33×105)×(43×π×2.03)=(1×105)×(43×π×r3)
⇒r3=1.33×2.03 mm3
⇒r=2.199 mm≈2.2 mm.