13.13 A gas in equilibrium has uniform density and pressure throughout its volume. This is strictly true only if there are no external influences. A gas column under gravity, for example, does not have uniform density (and pressure). As you might expect, its density decreases with height. The precise dependence is given by the so-called law of atmospheres

n2 = n1 exp [ -mg (h2h1)/ kBT]

where n2, n1 refer to number density at heights h2 and h1 respectively. Use this relation to derive the equation for sedimentation equilibrium of a suspension in a liquid column:

n2 = n1 exp [ -mg NA ( ρ - ρ' ) (h2h1)/ ( ρ RT)]

where ρ is the density of the suspended particle, and  that of surrounding medium. [NA is Avogadro’s number, and R the universal gas constant.] [Hint : Use Archimedes principle to find the apparent weight of the suspended particle.]

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    Payal Gupta | Contributor-Level 10

    5 months ago

    13.13 According to law of atmospheres, we have

    n2 = n1 exp [ -mg (h2h1)/ kBT] ….(i)

    where n1 is the number of density at height  h1and n2 is the number of density at height h2

    mg is the weight of the particle suspended in the gas column

    Density of the medium = ?

    Density of the suspended particle = ?'

    Mass of one suspended particle = m'

    Mass of medium displaced = m

    Volume of the suspended particle = V

    According to Archimedes's principle for a particle suspended in a liquid column, the effective weight of the suspended particle is given as:

    Weight of the medium displaced – weight of the suspended particle = mg – m'g

    = mg- V ?'g = mg –

    ...more

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