W. E. Sanford
Leonard F. Konikow
1998
<div class="t m0 x2 h4 y4 ff1 fs3 fc0 sc0 ls0 ws0"><p>We appreciate the opportunity to continue a dialogue on solute-transport modeling issues and perhaps to clarify some of our original concerns. It appears to us that Holzbecher [this issue] fails to consider the physical implications of groundwater flow and solute transport along no-flow boundaries. A no-flow boundary coincides with a streamline along which the fluid velocity is generally nonzero. Because the velocity is nonzero, both advective and dispersive transport processes can be operative along a no-flow boundary.</p></div>
application/pdf
10.1029/98WR02189
en
American Geophysical Union
Reply to comment by E. Holzbecher on "Constant-concentration boundary condition: Lessons from the HYDROCOIN variable-density groundwater benchmark problem"
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