Multiple surveys were conducted before and after storm surge at four beach sections,Sediment samples were analyzed and numerically simulated for understanding the characteristicsof becach reaction to storm surge and morphological evolution ,The results show that the sediment sources in this area do not increase in amount;the beach is basically stable in normal weather.While in gale weather,sediment from Yellow River and the eroded matters from the bank becomes a part of the sediment sources.The northem beach of Xiaoqing estuary is eroded seriously, while the southern beach is overall stable,Thw tidal creeks changed from the northern beach are transported greatly sea-ward and the inshore sediment becomes sandy,while that of the southem beach becomes silty,The sand transporting capability is almost 100 times of that in nomal weather. Human activities and big storm surges are the main reasons for the beach evolution.