Cold water can dissolve less salt than can hot water. Therefore, you would reach the saturation point faster with cold water.
I would think that its the saturation of clouds as if its cold surely the water vapour can condense and turn to rain or another form of precipitation.
A change of state will occur.
I do not Know either.
temperature affects the solubility of a substance..benzoic is poor in cold water because it is only slightly soluble in water..in order for it to reach the point of saturation, heat must be applied..heat acts as a catalyst..
Saturation and condensation are more likely to occur on a cold day. The temperature in the air is increased by the process of moisture condensation.Ê
Cold water can dissolve less salt than can hot water. Therefore, you would reach the saturation point faster with cold water.
I would think that its the saturation of clouds as if its cold surely the water vapour can condense and turn to rain or another form of precipitation.
Approx. 7,2 g at 20 0C.
This is the point at which saturation occurs. This is also signifies 100% relative humidity. If you want to find out how close it is to reaching saturation, all you have to do is find actual vapor pressure (found by temp.), and saturation vapor pressure(found by dewpoint). You can look online for conversion charts. Once you find them, plug them into this equation: actual vapor pressure/saturation vapor pressure x 100%. Your answer should be a percentage. If it's around 60-80 percent, then you know it's cold, and there is high humidity; thus, saturation is likely to occur. If it's around 10-30 percent, then you know the humidity is low and saturation is not likely occur. Warm weather= low humidity Cold weather= high humidity.
The zone of saturation and the water table share two zones of ground water.
Oil-WaterSWL = 0.2 SWCR = 0.22 SOWCR = 0.2 KRO = 0.9 KRW = 1 SORW = 0.2 KRORW = 0.8Saturation table end-point scaling (SWCR, SGCR, SOWCR, SOGCR, SWL)SWCR - critical water saturation (that is the largest water saturation for which the water relative permeability is zero)SOWCR - critical oil-in-water saturation (that is the largest oil saturation for which the oil relative permeability is zero in an oil-water system)SWL - connate water saturation (that is the smallest water saturation in a water saturation function table)Relative permeability end-point scaling (KRW, KRG, KRO, KRWR, KRGR, KRORG, KRORW)KRW - relative permeability of water at maximum water saturation parameterKRO - relative permeability of oil at maximum oil saturation parameterKRWR - relative permeability of water at residual oil saturation (or residual gas saturation in a gas-water run) parameterKRORW - relative permeability of oil at critical water saturation parameter
A change of state will occur.
critical water saturation (sometimes called Irreducible water saturation) defines the maximum water saturation that a formation with a given permeability and porosity can retain without producing water. This water, although present, is held in place by capillary forces and will not flow. Critical water saturations are usually determined through special core analysis.The critical water value should be compared to the reservoir's in-place water saturation calculated from downhole electric logs. If the in-place water saturation does not exceed the critical value, then the well will produce only hydrocarbons. These saturation comparisons are particularly important in low permeability reservoirs, where critical water saturation can exceed 60% while still producing only hydrocarbons.
Evaporation will occur on any surface having moisture on it, provided that the saturation or dew point has not reached 100% (i.e., the point at which the air has achieved the maximum amount of water vapor that it can hold).
warm air
Because clouds occur when water condenses from water vapour to tiny water droplets. Water condenses when it is cold enough, and higher up in the atmosphere, it is colder.