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The water will condense forming dew.
When AIR RISE THERE IS DECREASE IN PRESSURE WITH ELEVATION AT TEMPRATURE REMAIN SAME OF ATMOSPHERE UPTO 11 KM AND THE PARCEL OF AIR IS EXPAND AND IN TURN THE AIR CONDENSE TO FORM PRECIPITATION.
The air needs to be cooled, the amount depending on how much water vapour is in it. When it's cooled sufficiently the water vapour will condense on solid things as water, or become very small droplets (fog/cloud). When this happens in the early mornings we call it dew, and the temperature at which the water will condense is known as the dewpoint.
The percentage of oxygen in air is 21%.
The dew point is the temperature at which water will condense out of the air. If the dew point were above the temperature, that would mean that some of the water vapor in the air should have already condensed out. In such a situation, the excess water WOULD condense out, lowering the amount of water vapor and consequently the dew point.
As air molecules are cooled, they condense and form a liquid, and if cooled even further, will form a solid.
The water will condense forming dew.
The air needs to be cooled, the amount depending on how much water vapour is in it. When it's cooled sufficiently the water vapour will condense on solid things as water, or become very small droplets (fog/cloud). When this happens in the early mornings we call it dew, and the temperature at which the water will condense is known as the dewpoint.
There must be moisture in the air. When cooled, the water vapor in the air becomes liquid water- but if there is no moisture, then it cannot condense.
water vapor is different from other gases that make up air because it condenses out of air that has cooled
Because the gasses are compressed and cooled to -200 degress
A homogeneous mixture of gases (air) can be separated by fractional liquefaction. The mixture is gradually cooled, with the gases being separated by differences in boiling point.
nitrogen =78% oxygen=21% remaining 1% other gases like carbon dioxide and inertgases
air is separated through the process of fractional distillation this is where the gasses are cooled until they become a liquid. then the liquids are heated the lighter gasses boil first and evaporate then condense back into a liquid.
A homogeneous mixture of gases (air) can be separated by fractional liquefaction. The mixture is gradually cooled, with the gases being separated by differences in boiling point.
The rock will have little holes.
Any water vapour in the air, even on a warm day, will condense on the chilled surface of the glass.