The temperature of the water of a pond is $0^{\circ} C$ while that of the surrounding atmosphere is $-20^{\circ} C$. If the density of ice is $\rho$, the coefficient of thermal conductivity is $k$, and the latent heat of melting is $L$, then the thickness $Z$ of the ice layer formed increases as a function of time $t$ as:

  • A
    $Z^{2}=\frac{60 k}{\rho L} t$
  • B
    $Z=\sqrt{\frac{40 k}{\rho L} t}$
  • C
    $Z^{2}=\frac{40 k}{\rho L} \sqrt{t}$
  • D
    $Z^{2}=\frac{40 k}{\rho L} t$

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