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.