(d) all of the above
Reason — Uses of mercury as a barometric liquid are —
- The density of mercury is greater than that of any liquid, so only 0.76 m of the height of mercury is needed to balance the normal atmospheric pressure. Use of other liquids will require a much longer tube.
- The vapour pressure of mercury is negligible, so the vapours in the Torricellian vacuum do not affect the barometric height.
- Mercury neither wets nor sticks to the glass tube, therefore it gives an accurate reading.