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Density of water in solid state i.e. ice increases from 0oC to 4oC, where it has maximum density.
Ice has a cage-liked structure with lots of vacant spaces in between because of extensive hydrogen bonding between the water molecules. When the temperature increases, this structure collapses as the hydrogen bonding starts to break and as such the water molecules occupy the void spaces thereby increasing the density.
Beyond 4oC, the ice melts completely.

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Q: In what temperature range does density of water increases with temperature?
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