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<p>which typically are both quite small quantities. Unconfined aquifers have storativities (typically called <a href="page.php?w=Specific_storage">specific yield</a>) greater than 0.01 (1% of bulk volume); they release water from storage by the mechanism of actually draining the pores of the aquifer, releasing relatively large amounts of water (up to the drainable <a href="page.php?w=Hydrogeology">porosity</a> of the aquifer material, or the minimum volumetric <a href="page.php?w=water_content">water content</a>).</p>

<p><big> Isotropic versus anisotropic </big></p><p>
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