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The temperature of the ice salt mixture is determined by the percentage of salt mixed with the ice, such as the amount of salt used in ice, the minimum temperature can reach -21.
Ice is a crystalline formation formed by the orderly arrangement of water molecules, which are linked together by hydrogen bonds to form a very "open" (low-density) rigid structure.
The spacing between the O—O nuclei closest to the water molecule is about 109°, which is very close to the 109°28 bond angle of an ideal tetrahedron. However, the O-O spacing of each water molecule that is only adjacent and not directly bound is much larger, and the farthest one should be reached. Each water molecule can combine with 4 other water molecules to form a tetrahedral structure, so the coordination number of the water molecule is 4.
Ice is a colorless and transparent solid, a product formed by liquid solidification, condensed by a freezing environment, and liquefied and dissolved at high temperatures, which is a normal natural phenomenon that can be formed naturally or artificially.
The molecules are mainly bonded by hydrogen, but there are also van der Waals forces, and the lattice structure is generally hexagonal, which is less dense than water. However, there can also be other lattice structures at different pressures.
Ice crystals are structures in which water molecules are regularly arranged in a hexagonal shape. After heating, first of all, a water molecule detachs from the crystallization and begins to move freely, and this water molecule does not return to its original position, resulting in distortion of the crystal. Once the crystals are distorted, they will gradually expand, and eventually the entire crystals will decompose and become liquid.
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It is related to the concentration of the salt solution, in general, if the salt solution contains 20% salt, its freezing point will be reduced to -16
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If you mix ice and salt in a ratio of 3 to 1, it becomes what is called a refrigerant, and it can reduce the temperature.
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At. Standard case.
The lowest can be -18
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The freezing point decreases rapidly when salt is added to the ice, around 7. So there is ice backmelting. The temperature of the ice salt mixture is determined by the percentage of salt mixed with the ice, such as the amount of salt used in ice, the minimum temperature can reach -21.
Ice salt, refers to a mixture of ice and salt solution. A common icing salt is a mixture of ice and a sodium chloride solution. Ice salt mixtures are an effective chilling agent.
When salt is mixed with crushed ice, the salt dissolves in the ice and becomes endothermic, lowering the temperature of the ice. When ice salts are mixed together, they will greatly accelerate the melting rate of ice, and when the ice melts, it has to absorb a lot of heat; The dissolution of salt also absorbs the heat of dissolution. It can absorb a large amount of heat in a short period of time, so that the temperature of the ice-salt mixture drops rapidly, and it is much cooler than that of ice alone.
Related information
The cooling principle of the ice salt bath is related to the decrease in the freezing point of the solution. When salt and ice are evenly mixed together, the ice melts slightly into water due to the absorption of ambient heat, and the salt dissolves when it meets water, so that the surface water forms a concentrated salt solution. Because the freezing point of the concentrated salt solution is lower than that of pure water, the concentrated salt solution and ice coexist in the system.
Therefore, the temperature of the system must drop in order to maintain this coexistence (the coexistence temperature of the concentrated salt solution and ice should be lower than the freezing point of pure water). This will cause more ice to melt into water to dilute the concentrated salt solution, reducing the temperature of the system due to a large amount of endothermy during the melting process.
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The temperature of the ice brine can reach as low as -18 degrees Celsius under the standard standard.
The ice salt water is lower than ice water, reaching sub-zero condensation temperatures. Sodium chloride solution is commonly used.
It can also be calcium chloride solution, etc. It is convenient to use a circulating cooler to achieve the purpose. When the brine freezes, ice crystals will form locally and gradually expand, causing the salt solution to precipitate, resulting in local solution concentration.
Elevated, while the frozen part does not contain salt. <
The temperature of the ice brine can be as low as -18 degrees Celsius under standard conditions. The ice salt water is lower than ice water, reaching sub-zero condensation temperatures. Sodium chloride solution is commonly used, but it can also be calcium chloride solution, etc.
A circulating chiller can be used to achieve the purpose conveniently. When the brine freezes, ice crystals will form locally and gradually expand, causing the salt solution to precipitate, resulting in an increase in the concentration of the local solution, while the frozen part does not contain salt. This phenomenon occurs at the freezing point, and the water turns into ice salt because of the search for a large letter to melt the ice because of the crystalline structure of the ice.
It is covered by a thin layer of water in which the salt dissolves. When any substance is dissolved in water, it will lower the freezing point of water, the freezing point of water is 0 Water is salted, the temperature of the brine can be reduced to below zero, within a certain range of salinity, with the increase of the amount of salt, the temperature of the water can be reduced to a lower temperature before freezing, but after reaching a certain salinity, with the increase of salinity, the freezing temperature of the brine will increase.
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The freezing temperature of the brine depends on the concentration of the brine.
For example, the saltiness of the seawater is very high, which lowers the freezing point of the seawater. Freshwater freezing is at 0 degrees Celsius, with a freezing point of water containing 10 degrees of salinity. And the freezing point of water with 35 salinity is.
The average salinity of the seawater in the oceans of the earth is, therefore, the freezing point of the seawater is around the limit.
The higher the salt content of the brine, the lower its freezing point.
In general, the higher the concentration of brine, the lower its freezing point; As a result, the refrigeration and ice industries have prepared highly concentrated brine (calcium chloride.
It is used as a low-temperature refrigeration carrier, but when the concentration exceeds a certain critical value, it leads to another problem: the solubility of the salt solution.
Relationship with temperature.
The higher the temperature, the greater its solubility; Conversely, the lower the temperature, the lower its solubility.
All kinds of salt solutions have their own different physical characteristics, concentration and temperature constitute their own different crystalline areas, when a high concentration of the solution cools down to a certain low temperature point (close to its crystallization area), the solution will precipitate the salt crystals corresponding to its (temperature solubility) extra salt crystals, so the concentration of the prepared salt solution should grasp an appropriate value, which not only meets the low temperature requirements of the working conditions but does not freeze, and does not make the salt precipitation, and will not cause waste of cost.
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The freezing temperature of the brine depends on the concentration of the brine.
Seawater, for example, has a high salinity that lowers the freezing point of seawater. The freezing point of fresh water is 0 degrees Celsius, the freezing point of water with 10 salinity is 0 5, and the freezing point of water with 35 salinity is 1 9.
The average salinity of the seawater in the earth's oceans is 34 48, and the freezing point of the seawater is about 1 9. The higher the salt content of the brine, the lower its freezing point.
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The freezing temperature of the brine depends on the concentration of the brine.
Seawater, for example, has a high salinity that lowers the freezing point of seawater. Freshwater freezes at 0 degrees Celsius, the freezing point of water with 10 salinity is 0 5, and the freezing point of water with 35 salinity is 1 9.
The average salinity of the oceans on Earth is 34 48, so the freezing point of the sea is around 1 9. The higher the salt content of the brine, the lower its freezing point.
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