How much heat is being drawn when water vaporize?

In summary, In summary, a fan using wind at 25C with relative humidity of 40% can evaporate 10 grams of water.
  • #1
enth
12
0
Hello,

So, I'm not much of a physicist but I thought that at least this question will be simple enough to answer with some internet browsing... though it seems apparently that I can't tell my left from my right... :P

I have a bowl of water at room temperature (25 C). I blow at it with a fan who transports wind at say 25C with relative humidity of 40%.
And now I'm trying to figure out what amount of energy have disappeared from the liquid if say 10 grams were evaporated...



I read in wikipedia all about latent heat and heat of vaporization, but I still can't really figure much out.
Thank you very much, I know its fairly rudimentary question.
:)
 
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  • #2
Welcome to Physics Forums.

Heat of vaporization might be given in terms of Joules per gram, and you have 10 grams of water that evaporated. So it's a straightforward multiplication to get the energy change.
 
  • #3
total heat = mass x specific heat of vaporization. just plug it in. now if you want to account for the heat that's used by the fan, that gets tricky but let's assume its negligible so its still an easy equation.
 
  • #4
chill_factor said:
total heat = mass x specific heat of vaporization. just plug it in. now if you want to account for the heat that's used by the fan, that gets tricky but let's assume its negligible so its still an easy equation.

it's referred to as latent heat, I believe, if anyone wants to look it up.

Actually, the devil is in the detail in this situation. It is true that the amount of heat needed to vaporise 10g of water is easily calculated but the rate of cooling and the final temperature reached will depend on humidity and air speed (and the total mass of water you started with).

There is a quaint piece of equipment called a Wet and Dry Bulb Thermometer which can be used to measure air humidity. It is just what the name suggests and the wet bulb is wrapped in wet cloth. You whirl it around in the air and note the difference in temperature between the wet bulb and dry bulb. In highly saturated air the temperature difference will be small but, in very dry air, the temperature difference will be significant as the wet bulb cools down. There will be a table, printed on the back, to let you work out the humidity from the two readings.
 
  • #5
Thank you for your answers, but here is the thing that got me stuck-
Vaporization occurs when the surface molecules of the water receive energy from the air, allowing them to escape.
Latent heat of water vapor, as far as I understood (and please correct if I'm wrong) is the entire energy that water molecule posseses and with which it leaves the liquid system.
Meaning, Latent Heat=Energy taken from water+Energy taken from air. So how can I calculate only the energy which left the water?








edit: How much energy does a gram of 25C water (or any material really) carry?
Should the count be from freezing point (0C) or maybe from absolute zero?
Or am I completely off-base here?
 
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  • #6
The water will lose heat or gain heat from the air, depending on the temperature difference (could be either way).

The reason that heat is lost is that it is the faster water molecules (the ones with way above mean KE) that will escape. This means that the mean energy (temperature) reduces.

With a covered (insulated) container, the final situation will be that air and water end up at the same temperature and the vapour pressure in the air is the same as the vapour pressure on the water surface - the humidity will reach a steady value and as many molecules will land on the surface as leave the surface.

If there is a current of new air over the surface of the water, many of those faster water molecules which have made it into the air will be carried away, along with their 'above-mean' KE so the water temperature will continue to drop until, as before, the vapour pressures on either side of the boundary are the same.

For most thermodynamic problems like this, you are only interested in changes of energy and not absolute energy because absolute energy is not really relevant. (Who cares about the energy needed to bring your gram of water fro 0K to room temperature?)
 
  • #7
sophiecentaur said:
The water will lose heat or gain heat from the air, depending on the temperature difference (could be either way).
The temperature difference is zero:
enth said:
I have a bowl of water at room temperature (25 C). I blow at it with a fan who transports wind at say 25C with relative humidity of 40%.
 
  • #8
Redbelly98 said:
The temperature difference is zero:

But only at the start. The water will cool down. The energy needed to evaporate the water will come from the Air. The air will have thermal energy (KE of randomly moving fast molecules, which have an RMS speed of about 500m/s) and a very small amount of KE die to the total mass moving slowly (say 2m/s - and I think that only relates to the molecules near the surface). The only significant source of energy will be the thermal energy of the Air.

So the total energy involved will be mass X latent heat of vaporisation and it will all have to get there by cooling the air. If you want to work out the rate of cooling then that's a different problem - a bit harder.
 
  • #9
Okay, at first I was thinking the 25C air would maintain the water at the same temperature. But it makes sense that the water temperature would drop to some lower value, and the air would actually maintain that lower temperature for the water.
 
  • #10
I always like to tackle things like this from the Energy point of view. The energy for this, in the long run, must come from the air. Whatever the source of the energy, the latent heat of vaporisation is the same value.
The time factor is a much more difficult thing to discuss. It would relate to air speed and would be very non-linear as the surface would form wavelets, which would change the surface area plus the air flow. The rate of evaporation would be related to the final temperature of the water.
 
  • #11
Hmm...
Thank you, I think that I almost understand you. So if I want to know what the temperature of the (25C) water would be after 10g were evaporated, I should multiply the amount of water (0.01 kg) by the latent heat of evaporation (2257 kj/kg for water) which would give me the result of 22.57 kj, and... umm...
Not sure what next. :P
 
  • #12
Then: Heat supplied will be
Total mass X shc X temp drop
Equate the two and solve for unknown.
 
  • #13
So...
22.57kj= 22570 j

22570(j)=10(g)*4.186(j)*X(C)?

22570/41.86=X
x=539?


I obviously screwed the conversion somewhere...

PS-4.186 (j/g) is the specific heat of water...


PS2-
Uhh... Actually on second thought, I think that this is a misunderstanding problem and not a conversion one.
We have the value of the ENTIRE heat a water molecule possesses in order to become vapour (22.57).
We also have the values for energy required to raise this molecule by 1C (41.86).

But the formula you cited (Heat Added(Q)=Specific Heat(C)*Mass(m)*Change in temperature (Delta T))- Has 2 variables. Change in temperature and Heat ADDED (so that the molecule would have its ENTIRE energy).

Therefore...Uhhh... well I'm not sure about the formula I should make.

I hope that I was understood.
Sorry for holding the rest of the class, I've always been like this. XD
 
  • #14
I'm not sure exactly what your thought experiment consists of; it may not be realistic. The 10g of water can't 'contain' enough thermal energy for it to evaporate on its own. I think that's why you got a dodgy answer. It implies that the water needs to 'lose 540 degrees Celcius - the most it can lose is 300 and it'll be at Zeero K! haha
There must be some other source of heat (the rest of the water, the air, the Sun or a heater) to make the 10g evaporate.
 
  • #15
Ummm...
But are you sure that the entire use of the formulas was correct?

Don't we have two unknowns here?
'Change in temperature' and 'Heat added'?
How can we equate Q(Heat Added) to the overall heat of the system (the vapor molecules)? One is only a part of the other.


Thank you.
 
  • #16
enth said:
Ummm...
But are you sure that the entire use of the formulas was correct?

Don't we have two unknowns here?
'Change in temperature' and 'Heat added'?
How can we equate Q(Heat Added) to the overall heat of the system (the vapor molecules)? One is only a part of the other.


Thank you.

I don't know that the simple formula for latent heat of vaporisation holds over all temperatures (particularly when sublimation comes into it. Also, the SCH of water changes with temperature.
But the general principle holds and the experimental details are so vague that I reckon my conclusion is valid.
 
  • #17
Ok, so if my scenario is unrealistic, what is a realistic scenario then(when the water isn't hot so it's not the source of the energy)?
Why is it that when I'm in a room that shows around 25C on the thermometer and I blow a fan over a glass dish (or a towel) with little water- the water dissapears?
 
  • #18
Heat gets there from elsewhere because the room temperature drops.
 
  • #19
I see...
Well, I suppose that the heat comes from the air. So, are you saying that in a room temperature if I evaporate half a cup of water by blowing air, the temperature of the remainding water would not change?
 
  • #20
In an infinite room, the temperature of the water will drop until the latent heat times the mass lost per second is balanced by the rate at which heat goes from room to water.
 
  • #21
A quick question. In this infinite room you mention, is the reason that all of the energy for evaporation comes from the air and not from air+water, is because we use more mass of air, thus say 1 ton of air at 25C (blown over the bowl) will contain more energy than 1 kg of water at 25C?
 
  • #22
The total amount of energy is not relevant. In thermodynamics, what counts is the energy available due to temperature difference / change. So there is a lot of energy available for a difference in temperature of just a couple of degrees if there is a large mass of air ('infinite'). The air temperature change will not be noticeable whilst energy goes into the water to supply the latent heat. Of course, this latent heat will also be supplied by the initial drop in temperature of the water but it is only a small proportion of the total needed.
Is that clearer?
 
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  • #23
sophiecentaur said:
Is that clearer?

I think so, thank you.



Ok, So now that I'm trying to figure out the rate at which the colder water gains heat from the environment, should I use this formula: Heat conduction Q/ Time = (Thermal conductivity) x (Area) x (Thot - Tcold)/Thickness ?

(the bowl is 50cm in diameter and 10 cm deep(thickness), filled with water whcih thermal conductivity is 0.58 W/m C, water temp is let's say 20C and air is 25).
Thus 0.58*0.05*5/0.01?
 
  • #24
It's got to be harder than that. The surface is where everything is happening but how is the heat getting into the water? Is it through the container walls (e.g. blackened copper) or is it only getting there through the surface? (Polystyrene basin)
There are too many variables to be certain of the final temperature and the only way to work it out would be to do some experiments.
 
  • #25
No no, I'm talking about an insulated bowl where the only contact is between the air and the surface of the water.
Basically what I'm aiming for is what I suppose a classical thermodynamics problem per the scenario you suggested.
My bowl is completley hypothetical and in perfect environment, so like you said, it is already in a stage where it has lost its inital temperature and now is in equilibrium between heat lost and heat gained.
So my first step is to figure out what heat is being gained.
 
  • #26
So you've decided to go for the hardest one!
I have one more awkward question for you, though. Is the air stationary or moving? As soon as it moves, the convection will take over as the main heat transfer mechanism, I think.
Boy. This is difficult. The arm waving bit is easy but the quantitative stuff isn't.
 
  • #27
Lol, actually I thought this is the easiest option. What did you mean that is easier then?
:P
 
  • #28
I thought that you could have calculated the heat getting into a blackened container from surrounding air easier than needing to work out what's happening right on the surface. After all, wouldn't there be some sort of temperature gradient at the surface? Perhaps not, as the container is insulated.
I must admit, I'm getting into 'problem fatigue' haha.
 
  • #29
LOL, thank you for the effort. I know its not much, but I click every commercial link here every time I get in...:P

Well, for starters let's go your way. I assume that the blackened body is either water or a material containing waters heat conductivity properties.
Regarding your previous question, eventually of course I want to know what happens with moving air (which evaporates water from an insulated bowl), but first let's say that the air is still.
 
  • #30
Looking at your original problem (without the blackened container to help with the heat supply) I did find a link last night (but went to bed and forgot where I found it. It gave a value for heat transfer at an air interface for still air - about 20W/msquared/degreeC (plus or minus quite a lot)
I'm trying to get my head around how to relate this to the rate at which water can evaporate and the resulting actual temperature difference that it will settle at. I can't get back to this thread for a few days but I will keep thinking.
 
  • #31
enth,

When you say a bowl of water is at such-and-such a temperature, that effectively specifies the average kinetic energy in each molecule. At any instant, though, some will have more, some less, according to a standard probability distribution.
The more energetic ones may have enough energy to escape the bowl and become vapour.
At the same time, the water vapour molecules in the air are bouncing around, gaining and losing energy. Some lose so much that they get caught by the water.

When these two processes are in balance, no net evaporation or condensation occurs.
Make the air a bit drier and fewer are available to recondense, so net evaporation does occur. Make the water a bit warmer and more are available to evaporate.
So at a given water temperature, there's a certain density of vapour above it (the saturation vapour pressure at that temperature) at which the system is in equilibrium.

In all cases, evaporation cools the water and condensation heats it.

The fan in your model is there purely to ensure a steady supply of air at the given temperature and humidity (otherwise the air just above the water gets saturated and cold). Similarly, the surface layer of the water will cool first, inhibiting further evaporation, but as long as it's above 4C convection should kick in and redistribute the heat.

Based on the above, you can do the calculation exactly as SophieC said.
temperature drop in bowl = heat required to vaporise lost water / thermal capacity of remaining water.

Once the water starts to cool, it will be cooler than the air above. This means some heat will flow from the air to the water. As a result, the temperature drop will not be quite as great.
 

1. What is the heat of vaporization for water?

The heat of vaporization for water is 2,260 kJ/kg at a temperature of 100 degrees Celsius and atmospheric pressure. This means that it takes 2,260 kJ of energy to convert 1 kg of liquid water into water vapor at its boiling point.

2. How does the heat of vaporization affect the boiling point of water?

The heat of vaporization is directly related to the boiling point of water. As the heat of vaporization increases, the boiling point of water also increases. This is because a higher amount of energy is required to break the bonds between water molecules and convert them into vapor at a higher temperature.

3. Does the heat of vaporization change with altitude?

Yes, the heat of vaporization for water decreases with increasing altitude. This is because the atmospheric pressure decreases at higher altitudes, making it easier for water molecules to escape into the air. As a result, less energy is needed to vaporize water at higher altitudes.

4. How does the heat of vaporization differ between water and other liquids?

The heat of vaporization for water is relatively high compared to other liquids. This is due to the strong hydrogen bonds between water molecules, which require a significant amount of energy to break. Other liquids with weaker intermolecular forces have lower heat of vaporization values.

5. Can the heat of vaporization of water be changed?

No, the heat of vaporization for water is a physical property that is constant at a given temperature and pressure. However, it can be affected by external factors such as altitude and impurities in the water. Additionally, the heat of vaporization can be changed by altering the temperature and pressure conditions under which water is vaporized.

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