I've come across the Wikipedia article on Rayleigh Scattering and it quotes that
In detail, the intensity $I$ of light scattered by any one of the small spheres of diameter $d$ and refractive index $n$ from a beam of unpolarized light of wavelength $λ$ and intensity $I_0$ is given by
$$I = I_o \left(\frac{1 + cos^2\theta}{2R^2}\right)\left(\frac{2\pi}{\lambda}\right)^4\left(\frac{n^2-1}{n^2+2}\right)^2\left(\frac{d}{2}\right)^6$$
In another article, it says that a hydrogen-dominated atmosphere exhibits stronger Rayleigh scattering effect as compared to an atmosphere which is oxygen-dominated. From the formula quoted above, I can't see how is this so. In any way, the "particle size" of a hydrogen molecule is probably less than that of an oxygen molecule. If $d$ was the factor, it would have said that the intensity of the scattered light should have been lower, contradicting the statement above.
Is there another way to think about this problem and possibly explaining the difference in the scattering effect in two different atmospheres?