yes because the pure water does not contain the nuclei that it needs to freeze
my guess is that it needs a little extra engery to begin the formation of the ice crystals. once it its started, the crystals build on each other
flash freezing works when water is cooled below its freezing point to form supercooled water. when ice is added ice crystals instantly form around the ice to create a flash freeze
It would be lower.
A supercooled solution is something solid,cold, and made up of alchol.
Sea water will not freeze.
I know it sounds a little stupid, but supercooling is when water remains a liquid while it is below freezing point. Note, only some waters can do this.
Yes, with the addition of a solute or by increasing pressure water can be kept liquid below its normal freezing point. Water can also be supercooled, but will freeze instantly if it is disturbed.
yes, i don't have any way 2 prove it 2 u but the answer yes.
It works if the water is supercooled, and the shock provides a nucleation site and a variance in pressure.
ice
I believe hot water freezes faster because it is supercooled. Cold water is non-supercooled. When cold water freezes ice crystals form and float to the top, forming a layer of ice over the top of the water, so the layer of ice stops evaporation . While the hot water, which is probably no longer hot in the freezer,when it does freeze, it freezes throughout, creating more or less of a slush before freezing solid.
Supercooled.
no it is glaze
Graupel, also called soft hail or snow pellets, refers to precipitation that forms when supercooled droplets of water are collected and freeze on a falling snowflake.
In order for water to be supercooled, there must not be impurities that can act as nucleation sites within the water. Spring water should work, though tap water would more than likely need to be purified before it would be supercooled, as by reverse osmosis.
flash freezing works when water is cooled below its freezing point to form supercooled water. when ice is added ice crystals instantly form around the ice to create a flash freeze
Inside a cumulonimbus cloud air move up in what is called an updraft. If this updraft is strong enough, it can keep ice pellets suspended in the air. At these heights, temperaures are always very cold, however, droplets of supercooled water exist. These droplets consist of water that remains liquid below the normal freezing point and will freeze instantly if disturbed. These droplets freeze to the surface of the ice pellet, causing it to grow into a hailstone. Eventually, the hailstoen grows to heavy to remain suspended and falls to the ground.
The temparature at which supercooled water freeze is an important factor in cloud information.