If you assume the atmosphere is made of an ideal gas in isothermal equilibrium, and that it is not so thick that the gravitational acceleration changes significantly across it, the formula is: P(h)=Ce^{\frac{-\mu{}GM}{RTr^2}h} where h is the height, \mu is the molar mass of the gass, G is the universal gravitational constant, R is the molar gas constant, T is the temperature, r is the radius of the planet, and C is the pressure at the surface of the planet. Since one has to know the pressure at some height before one can determine this function, it cannot answer your question as to the appropriateness of the surface pressure you gave. However, other factors could be used to determine an appropriate surface pressure. Geochemically, the atmosphere has its current composition and volume due to the balance of the processes that add and remove gases from it (e.g. photosynthesis adds oxygen, oxidation (burning, rusting, etc.) removes it). Biologically, organisms (especially complex ones) usually only survive in a fairly narrow region of pressures and temperatures.
So, one must consider additional constraints in order to answer your questions. For example if one assumes that the total mass of the atmosphere is constant (with pressure as a function of height given by the equation above and gravity by the inverse square law), then reducing a planet's radius by a certain factor will increase the pressure at the surface by the (approximately) inverse square of that factor (e.g., r_{2}=\frac{r_{1}}{2} \Rightarrow C_{2}=4C_{1}). So, for the surface pressure to be 108.75 kPa the mass of the atmosphere would have to be about the same as the Earth's (for 1.1 times the radius and 1.3 times the mass and the same molar weight it would have to be the same within 1%, though I have no reason to believe that having the same mass of atmosphere is a realistic constraint)