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We cannot estimate exact permeability of the aquitard because we need the thickness of aquitard and difference in groundwater pressure between the aquifer and aquitard (Ostendorf et al. 2010).
Specific attention was paid on the flow across the aquitard aquifer interface, which is of concern if aquitard and aquifer have different pore water chemistry.
Recharge areas are shown in the aquitard layer to assist the discussion.
The mass transported between the aquifer and the aquitard is sensitive to the aquitard Peclet number, but less sensitive to the aquitard diffusion coefficient.
The top most aquitard is relatively thin and discontinuous along the section BB′.
The glacial deposits act as an aquitard potentially affording protection from surface-derived, mainly agricultural contaminants.
The AA method overestimates the mass transported into the upper aquitard when an upward advection exists in the upper aquitard.
Net to gross ratio within the aquifer [i.e., aquifer/(aquifer + aquitard ratio) within the gross aquifer unit].
The dip of the underlying aquitard was found to be relatively unimportant, at least for the range of values studied.
These formations are overlaid by loess deposits, which are characterized by low hydraulic conductivity and constitute an aquitard.
The clay layer (i.e., aquitard) has minimum thickness (<10 m) towards northern and north-eastern part of the basin.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com