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For a very small region of temperature, the density of water increases as the temperature increases:

For the table below, whole degrees are listed down the left hand side of the table, while tenths of a degree are listed across the top.

So to find the density of water at say 3.4 °C, you would first find the whole degree by searching down the left hand

column until you reach '3'. Then you would slide across that row until you reach the column labeled '0.4'.

The density of water at 3.4 °C is 0.999970 g/mL.

--0.0-----0.1-----0.2-----0.3-----0.4-----0.5-----0.6----0.7----0.8----0.9------

00.9998410.9998470.9998540.9998600.9998660.9998720.9998780.9998840.9998890.99989510.9999000.9999050.9999090.9999140.9999180.9999230.9999270.9999300.9999340.99993820.9999410.9999440.9999470.9999500.9999530.9999550.9999580.9999600.9999620.99996430.9999650.9999670.9999680.9999690.9999700.9999710.9999720.9999720.9999730.99997340.9999730.9999730.9999730.9999720.9999720.9999720.9999700.9999690.9999680.999966

Referring to the table you can see that the density of pure water increases from 0 °C until it reaches a maximum somewhere between 3.8 °C and 4.4 °C and then decreases continually with any additional rise in temperature.

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12y ago

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