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Directory UMM :Data Elmu:jurnal:A:Advances In Water Resources:Vol21.Issue6.1998:

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Fig. 2. The conductivity of the bedrock as a function of depth. (a)Monotonously varying conductivity, equation (1)
Fig. 3. The flow domain. (a) The real domain R. (b) The simplified
Table 1. Combination of periodic solutions for the simple extreme cases
Fig. 5. Streamlines in a semi-space, that are induced by a simpleperiodic topography with superimposed ridges and valleys
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