Mankind activity and climate variety are the diplex factor of shallow groundwater decline in the valley area of Hutuo River. The questions are worth discussing that how the shallow groundwater changes from crude state to false state and what change the shallow groundwater in space and time has. After all,the discussion will provide the gist for mankind controlling their activities,self-restraining groundwater,and ensuring the harmonious relation between mankind and groundwater. This article chooses integrated index means,filters the disturbing index,and establishes the quantitative analysis system. On the base of the above,the disturbing degree of mankind activities to shallow groundwater is quantitatively analyzed. Results show that spatially,the disturbing degree decreases gradually from the west to the east in different ages; in view of the whole area,the disturbing degree increases from thewest to the east; and the disturbing degree increases from 0～0.4 to 0.2～1.0. Temporarily,the disturbing degree in the whole area increases along with time,but it is different in different areas. The disturbance of mankind activities to shallow groundwater goes through different stages.