2. Consider a simple model for earth's atmosphere by neglecting winds, convection and variation in gravity etc. The distribution of molecules is varying with height. Assume that the atmosphere is isothermal (at 273 K) and the average molecular weight of the atmosphere is 30 g/mol, the height below which half the molecules ie approximately is
(A) 3.5 km
(B) 4.2 km
(C) 5.4 km
(D) 6.7 km

(E) 8.1 km

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