Relative humidity increases
The temperature to which air must be cooled to reach saturation is called the dew point.
FeCI2 is a combination of iron and hydrochloride. This solution starts out as a yellowish green color. When the equivalence point is reach the solution turns to an orange brown color.
Highest point reached by a curve. Minima is lowest.
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Saturation point is a pint when no more solute can be dissolved in a solvent. The saturation point is directly related to the temperature. Increase in temperature results in increasing kinectic energy of molecules and hence can dissolve further. For example dissolve salt in cup of water, the salt with dissolve till certain point, stirring can can take you one step further but if you continue pouring salt in the same cup which has definite volume of water, you will reach to a point where no more salt will be dissolved. This point is the saturation point. Now put this cup on stove and you will see that supplying thermal energy (heat energy in transit), will dissolve the salt further.
Condensation
When a parcel of air is cooled to the temperature at which it is saturated, it has reached its dew point temperature. At the dew point temperature, the air is holding the maximum amount of moisture it can hold, and any further cooling will result in the formation of water droplets or condensation.
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As bromine is cooled, the particles comprising the bromine slow down and lose kinetic energy. Eventually, the particles come closer together, forming a liquid as the temperature decreases further. At the point where the bromine reaches its freezing/melting point, the particles will arrange into a solid structure.
supercooled
Technically, the freezing point of water is at 0oC. Water is most dense at 5oC, then if cooled further it would be solid at 0oC.
When the equivalence point is reached in a titration, the color of Fe2 changes because it reacts with the titrant to form a different colored compound.
Heat moves from the water to its surroundings when water is cooled below 0 degrees Celsius. This causes the temperature of the water to decrease further until it reaches its freezing point, at which point it will freeze into ice.
It continues to cool until it reaches it's boilng point. At which it will condense then cool further until it reaches it's melting point. It will then continue to cool until it's entropy is minized at absolute zero.
When liquid water is cooled, it contracts like one would expect until a temperature of approximately 4 degrees Celsius is reached. After that, it expands slightly until it reaches the freezing point, and then when it freezes it expands by approximately 9%
condensation Another question that follows: As an air mass cools to its dew point; relative humidity increases
When a liquid is cooled to its freezing point, it changes state from a liquid to a solid. The molecules within the liquid slow down and lose energy, causing them to form a more organized structure with a fixed shape and volume. This process is known as solidification.