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Hint: We know that the aqueous solution of sodium chloride is saline water/brine solution which was relatively high concentration of salt (which is usually sodium chloride) that takes place naturally on the crust; the surface of the Brine naturally takes place on the surface of the crust, the Earth, within brine pools on the ocean bottom.
Complete answer:
There exist a number of processes that can produce brines in nature. Seawater modification via evaporation results in the concentration of salts in the residual fluid; a characteristic geologic deposit known as evaporate can be produced as different dissolved ions reach the saturation states of minerals, typically halite and gypsum. The same process takes place at high latitudes as seawater, and it freezes, resulting in a fluid termed cryogenic brine. At the formation time, these cryogenic brines are by definition cooler compared to the freezing temperature of seawater and can also produce a feature, where cool brines descend by freezing the surrounding seawater.
It is a high-concentration resolution of salt \[\left( NaCl \right)\] in water \[\left( {{H}_{2}}O \right).\] In varied circumstances, brine might check with salt solutions variable from regarding \[3.5%\] (a customary concentration of brine, on the lower finish of resolutions used for brining foods up to regarding twenty sixth a typical saturated solution, betting on temperature. Lower levels of concentration of the answer area unit known by numerous names like fresh, briny water, and saline water.
Brine naturally happens on the Earth’s surface salt lakes, crust, and at intervals brine pools on the seabed. High-concentration brine lakes generally emerge because of the evaporation of ground saline water at high close temperatures. Brine has varied applications. Used as a preservative in meat-packing as in cured beef and pickling.
Note:
Remember that the brine cropping out at saltwater surface springs are called saline’s or licks. The contents of the dissolved solids present in groundwater vary highly from one to another location also in refrigeration and cooling systems, brines are area units used as heat-transfer media due to their low freeze temperatures or as vapour-absorption agents because they exhibit low force per unit area.
Complete answer:
There exist a number of processes that can produce brines in nature. Seawater modification via evaporation results in the concentration of salts in the residual fluid; a characteristic geologic deposit known as evaporate can be produced as different dissolved ions reach the saturation states of minerals, typically halite and gypsum. The same process takes place at high latitudes as seawater, and it freezes, resulting in a fluid termed cryogenic brine. At the formation time, these cryogenic brines are by definition cooler compared to the freezing temperature of seawater and can also produce a feature, where cool brines descend by freezing the surrounding seawater.
It is a high-concentration resolution of salt \[\left( NaCl \right)\] in water \[\left( {{H}_{2}}O \right).\] In varied circumstances, brine might check with salt solutions variable from regarding \[3.5%\] (a customary concentration of brine, on the lower finish of resolutions used for brining foods up to regarding twenty sixth a typical saturated solution, betting on temperature. Lower levels of concentration of the answer area unit known by numerous names like fresh, briny water, and saline water.
Brine naturally happens on the Earth’s surface salt lakes, crust, and at intervals brine pools on the seabed. High-concentration brine lakes generally emerge because of the evaporation of ground saline water at high close temperatures. Brine has varied applications. Used as a preservative in meat-packing as in cured beef and pickling.
Note:
Remember that the brine cropping out at saltwater surface springs are called saline’s or licks. The contents of the dissolved solids present in groundwater vary highly from one to another location also in refrigeration and cooling systems, brines are area units used as heat-transfer media due to their low freeze temperatures or as vapour-absorption agents because they exhibit low force per unit area.
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