7. Diffusion-sedimentation equilibrium of hydrosol particles was established at a height of 0.326 m. The sol particles are spherical and have a dispersion of 0.1 nm-1. The density of a part of the sol is 2.7 g/cm3, the density of water is 1000 kg/m3 at 298 K. How did the concentration of sol particles change at the specified height and by how many times?

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