In this work, a relationship between the role of NH and the properties of mineral oxides (α-FeO, α-AlO, CaO, and MgO) in the evolution of NO, SO, and NH has been established. It was found that the promotion effect of NH was more favorable for the formation of NO (or SO) and NH on acidic α-FeO and α-AlO due to acid-base interactions between NO with NH or between SO and NH, while this effect was weaker on basic CaO and MgO possibly due to their basic nature. The acid-base interaction (NO/SO with NH) overpowered the redox reaction (SO with NO) on FeO owing to its unique redox chemistry. However, the opposite was found on basic CaO and MgO for the formation of SO and NO. Under equivalent concentration conditions, the two synergistic effects did not further strengthen on FeO, CaO and MgO due to a competition effect. In NH-rich situation, a synchronous increase of SO, NO, and NH occurred on FeO. On acidic AlO, the favorable adsorption of NH on the surface as well as the existence of NO with an oxidizing capability synergistically promoted the formation of SO, NO, and NH.