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Most substances contract on freezing . H...

Most substances contract on freezing . However, water does not belong to this category. We know that water expands on freezing. Further , coefficient of volume expansion of water in the temperature range from `0^(@)C` to `4^(@)C` is negative and above `4^(@)C` it is positive . This behaviour of water shapes the freezing of lakes as the atmospheric temperature goes down and it is still above `4^(@)C`.
As the atmospheric temperature goes below `4^(@)C`

A

Cooled water at the surface flows downward because of its greater density

B

Cooled water at the surface does not flow downward and remains at the surface because its smaller density

C

Cooled water at the surface downward because of its density

D

Temperature of water in the lake reduces with depth

Text Solution

Verified by Experts

The correct Answer is:
B

At temperature below `4^(@)C` , temperature above is less as compared to below & thus water remain is it is due to higher volume at the upper surface.
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The density of wathr at 0^C is 0.998 g cm^(-3) at 4^C is 1.00 g cm^(-3) . Calculate the average coefficient of volume expansion of water in th etemperature range 0 to 4^C .

A: Density of water is maximum at 4^(@)C . R : Water has both positive and negative temperature coefficients of volumetric expansions depending on the temperature range.

Knowledge Check

  • Most substances contract on freezing . However, water does not belong to this category. We know that water expands on freezing. Further , coefficient of volume expansion of water in the temperature range from 0^(@)C to 4^(@)C is negative and above 4^(@)C it is positive . This behaviour of water shapes the freezing of lakes as the atmospheric temperature goes down and it is still above 4^(@)C . If the atmospheric temperature is below 0^(@)C

    A
    Ice will form from the bottom upward and the plants and animals in the lake will be displaced to the upper part of the lake.
    B
    Ice will form in a random manner throughout the volume of the lake and with passage of time , different segments of ice will join together to result in a collective ice mass
    C
    Ice will form from the surface downward and plant and animal life will survive in the water beneath
    D
    Water in the lake does not freeze. In fact, water in the atmospheric freezes and fall into the lake and floats on the surface of lake as ice.
  • Most substances contract on freezing . However, water does not belong to this category. We know that water expands on freezing. Further , coefficient of volume expansion of water in the temperature range from 0^(@)C to 4^(@)C is negative and above 4^(@)C it is positive . This behaviour of water shapes the freezing of lakes as the atmospheric temperature goes down and it is still above 4^(@)C . If the atmospheric temperature is below 0^(@)C and ice begins to form at t = 0 , thickness of ice sheet formed up to a time 't' will be directly proprotional to

    A
    `t^(4)`
    B
    `t^(2)`
    C
    `t`
    D
    `t^(1//2)`
  • When water at 0^(@)C freezes to form ice at the same temperature of 0^(@)C , then it :

    A
    absorbs some heat
    B
    releases some heat
    C
    neither absorbs nor releases heat
    D
    absorbs exactly `3.34 xx 10^(5) J//kg` of heat
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