In order to clarify the state and distribution of water in non-fermented frozen dough at different mixing times and during freezing storage， low-field nuclear magnetic resonance (LF-NMR) was used to determine the moisture state of dough and after freezing during the dough mixing process by farinograph. The results showed that: In the dough mixing process， the proportion of strongly bound water (A21) in the dough just after leaving 500 BU was the highest and the proportion of weakly bound water(A22) was the highest. At this time， the water binding state was the best， and the gluten was fully hydrated. Ice crystal pores with irregular shapes and uneven distribution appeared inside the dough with different stirring times after freezing. However， the A21 value of the dough that had just left 500 BU was still the highest after freezing， the number of internal ice crystal pores was small， and the area of ice crystal pores was small. The moisture binding state was better. Conclusion: The moisture binding state of the dough that just left 500 BU from the farinograph kneading process was the best， the gluten network structure was fully formed， and the mobility of internal water molecules was the lowest. After frozen storage， the moisture binding state of the dough that had just left 500 BU was still good， and the internal water molecules were relatively stable.