1989 Volume 33 Pages 43-48
To evaluate the role of non-homogeneous geologic condition on ground water runoff, spring discharge and electric conductivity of water (EC) were observed from April to December, 1988.
Although N and S spring are located very closely, each spring has different runoff pattern and EC value.
Considering the geologic condition, discharge and EC at N, S spring are estimated by multi-layer model.
It is indicated that ground water runoff system depeno on the depth of clay-layer between aquifiers.