Terzahi's basic differential equal for one dimensional consolidation of clayey solis is

- 1
  
  $\frac{δ u}{\partial t} = C_{v} \frac{δ u}{\partial z}$
- 2
  
  $\frac{δ u}{\partial z} = C_{v} \frac{\partial^{2} u}{\partial t^{2}}$
- 3
  
  $\frac{\partial^{2} u}{\partial t^{2}} = C_{v} \frac{δ u}{\partial z}$
- 4
  
  $\frac{δ u}{\partial t} = C_{v} \frac{\partial^{2} u}{\partial z^{2}}$

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