Correct Answer: (c) The density of water is maximum at 4°C.
Solution:The anomalous expension of water as it cools from 4°C to 0°C means that the density of water is greatest at 4°C. So the ice that forms in cold weather forms at the top of the water (where the less dense coldest water gathers) and then acts as an insulating barrier preventing the water underneath from getting much colder (because heat cannot escape).
• Most substances become denser as they cool down. Water does this too, but only down to 4°C.
• As water cools from higher temperature (e.g., 10°C) towards 4°C, its density increases. Colder, denser water sinks, displacing warmer, less dense water upwards. This process is called convection.
• This convection continues until the entire body of water reaches approximately 4°C. At this point, the densest water is at the bottom of the lake.
• However, as the water cools from 4°C down to 0°C (its freezing point), its density starts to decrease. Water at 3°C is less dense than water at 4°C, water at 2°C is less dense, and so on. Ice at 0°C is significantly less dense than water at 0°C or 4°C, which is why ice floats.
• Because water cooler than 4°C is less dense than water at 4°C, it remains near the surface once it cools below 4°C. It does not sink.
• This means that once the lake's temperature profile reaches 4°C throughout, further cooling only affects the surface layers. The surface cools from 4°C to 0°C and freezes, while the denser 4°C water remains undisturbed at the bottom.
• Convection currents stop effectively transferring heat downwards once the surface layer cools below 4°C.