$A$ stone of relative density $K$ is released from rest on the surface of a lake. If viscous effects are ignored, the stone sinks in water with an acceleration of

  • A
    $g(1-K)$
  • B
    $g(1+K)$
  • C
    $g\left(1-\frac{1}{K}\right)$
  • D
    $g\left(1+\frac{1}{K}\right)$

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