There is a growing concern regarding the environmental geological problems resulting from the over- exploitation of groundwater in the Beijing area. In response to this, active measures such as groundwater mining restrictions and artificial recharge have been implemented since 2010 to address the severe groundwater shortage in Beijing. To further analyze the impact of the implementation of various water management measures on regional groundwater and land subsidence since 2010, this paper analyzes the dynamic evolution characteristics of regional groundwater during the period of 2010~2020. It utilizes long- term monitoring data, quantifies the contribution of various measures in decelerating the decline of groundwater levels, and investigates the deformation characteristics of soil layers under groundwater level recovery. The results show that: ① From 2010 to 2020, the rate of decline of groundwater levels in the plains slowed down. However, groundwater levels continue to decline in most areas of the alluvial plains, while experiencing a significant rise in the root fan, middle fans, fan margins, and some areas of the alluvial plains. ② In the Chaobai River basin, the significant rise in groundwater levels at the root, middle, and margins of the alluvial fan can be attributed to the artificial recharge of the Chaobai River; groundwater extraction restrictions are the main factors contributing to the significant rise in groundwater levels in other areas of the Beijing Plain; and the continuous decline in groundwater levels in the alluvial plain is primarily driven by the increase in domestic water use. ③ From 2010 to 2020, the third and fourth aquifer groups exhibit the most significant deformation layers, with deformation rates ranging from 11. 07 to 12. 80 mm/a. On the other hand, the first and second aquifer layers show rebound, with a maximum cumulative rebound of 5. 6 mm. ④ The dilation of soil caused by the rise of groundwater levels results in two types of deformation in the soil layers. The first type is elastic deformation, which occurs synchronously with the change in groundwater level. The second type is residual deformation, which lags behind the change in groundwater level. The results of this paper provide valuable technical support for understanding the effectiveness of different water management measures. These insights can contribute to the development of regional groundwater resource management strategies and the accurate prevention and control of subsidence.