There is a layer of snow $x \ cm$ thick on water,when the temperature of the air is $-\theta ^\circ C$ (less than the freezing point). If the thickness of the layer increases from $x$ to $y$ in time $t$,then the value of $t$ is given by:

  • A
    $\frac{(y^2 - x^2)\rho L}{2k\theta}$
  • B
    $\frac{(x - y)\rho L}{2k\theta}$
  • C
    $\frac{(x + y)(x - y)\rho L}{k\theta}$
  • D
    $\frac{(x - y)\rho Lk}{2\theta}$

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