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If $d$ is the depth of an aquifer through which water is flowing, then the relationship between permeability $K$ and transmissibility $\text{(also known as transmissivity)}$ $T$ is given by

  1. $T=K d$
  2. $T=K / d$
  3. $T=\sqrt{K d}$
  4. $K=\sqrt{T d}$

     

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