The interaction between the soil moisture balance of huge watershed scales and atmospheric has been shown to be capable of exhibiting very complicated dynamics depending on the climate, soil and vegetation conditions which control its parameters. Therefore, the purpose of the research is to study the relation between soil moisture and lagged soil moisture by the nonlinear soil moisture balance equation. To reconstruct the phase space of the equation by the time series method that can describe the hydrologic phenomena. It is shown that the phenomena of nonlinear dynamics equation will become quite complex, such as fixed point. limit cycle. and chaotic type of behavior.