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In cold countries, agricultural fields are watered during evenings. When atmosphere cools, this water also gets cooled. Then more heat is liberated. Thus this heat protects the seeds and plants from getting freezed. Water is used in the radiators of vehicles. Even though water receives a lot of heat from the engine, because of it's high specific heat capacity the water doesn't get heated fast.
To calculate the loading capacity of the buoyancy tank float in sea water, you need to consider the buoyancy force acting on the tank. This force is equal to the weight of the water displaced by the tank. You can use the formula: Buoyancy Force = Volume of the tank x Density of sea water x Gravity. With the given dimensions, you can calculate the volume of the tank and use the density of sea water (around 1025 kg/m^3) to find the loading capacity.
No, the specific gravity of sea water can vary depending on factors like temperature, salinity, and pressure. However, at standard conditions, the average specific gravity of sea water is around 1.025.
Yes, sea water expands when heated because the heat causes the water molecules to move faster and spread out, increasing the volume of the water.
Sea water is used to cool nuclear reactors in emergency situations when fresh water is not available. We usually find very pure water used in nuclear reactors as a primary coolant. This water stays quite pure and retains little radiation after shutdown and cooldown. But if an emergency situation arises and the "regular" primary coolant (the fresh water) is lost, it must be replaced with any water to cool the reactor. Sea water is better than nothing.
The usual cause of sea breeze is the difference in specific heat capacity between land and water Land heats and cools more quickly than water.
Land loses heat faster than the sea because water has a higher specific heat capacity than land. This means that it takes more energy to change the temperature of water compared to land. Additionally, water can circulate and mix, distributing heat more evenly and slowing down the cooling process.
63.9 ml per joules a second. In the arctic sea only.
i like to give a short application of specific heast energyland and sea breeze,air conditioners as a coolent, radiators ,
In cold countries, agricultural fields are watered during evenings. When atmosphere cools, this water also gets cooled. Then more heat is liberated. Thus this heat protects the seeds and plants from getting freezed. Water is used in the radiators of vehicles. Even though water receives a lot of heat from the engine, because of it's high specific heat capacity the water doesn't get heated fast.
the seawater smells
Sea water retains warmth even after sunset due to its high specific heat capacity, which allows it to absorb and hold heat from the sun during the day. Additionally, the depth of the ocean means that heat is distributed over a large volume of water, slowing down the cooling process. Factors like ocean currents and the insulation effect of the atmosphere also contribute to maintaining warmer temperatures in the water.
Land heats up more rapidly during the day compared to the sea due to its lower specific heat capacity. Land absorbs and releases heat quickly, while the sea has a greater capacity to store and release heat, resulting in slower temperature changes.
The property of water that helps produce sea breezes and land breezes is its high specific heat capacity. Water can absorb and release heat slowly, leading to temperature differences between land and water. During the day, land heats up faster than water, causing air to rise and drawing in cooler sea breezes. At night, the reverse happens, with land cooling faster than water and leading to land breezes.
It is important for aquatic life. Sea water does not heat too much with the sun heating it all day long. Thus, aquatic animals enjoy of a constant temperature in the sea.
A meadow will heat up faster than a pond because water has a higher heat capacity than land. This means that water can absorb more heat energy without a significant rise in temperature, whereas land will heat up more quickly due to its lower heat capacity.
Land warms faster than the sea during the daytime because land has a lower heat capacity than water. This means that land can heat up quicker when exposed to sunlight compared to water.