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Question number 127 is asking us about a person walking through the desert in the heat of the day wearing a bathing suit.
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We're asked in the first part of our question to find the rate at which the person's skin is heated up by the following four mechanisms.
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The first of these mechanisms is the heat of metabolic reactions within a person's body.
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This is where the energy is converted to heat underneath the person's skin and is acting to heat it up.
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So that's one of the sources of heat.
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The second source of heat is the heat from air convection within the desert that's acting to heat up the person's skin.
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One of the ways in which heat is transferred from one object to another is through convection.
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And so the person's skin will feel the heat by this method.
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Another method by which the person's skin will be heated up is by means of solar radiation.
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The sun in the sky definitely act to heat up the person's skin very well.
01:25
And the final source of heat will be the radiation from the environment, the environmental radiation.
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So we have our four sources of heat impacting this person.
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Let's see which one contributes most significantly.
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We're told that the rate at which the person's skin is heated by metabolic reactions is valued at 280 watts, so that rate is given to us.
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The heat from air convection is given to us via an expression of the following nature.
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The heat h is equal to k prime times the area of exposed skin, i'm just going to call a sub -skin, times the temperature of the air minus the temperature of the skin.
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We're given values for all of these terms.
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K -prime is valued at 54 joules per hour per degree celsius per meter squared.
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The area of skin exposed to the environment by this person wearing the bathing suit is 1 .4.
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Meters squared, the temperature of the air is valued at 47 degrees celsius, and the temperature of the person's exposed skin is 36 degrees celsius.
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Performing our calculations, we can cancel out the meters squared and the degrees celsius from our problem to get our answer in joules per hour.
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And the heat from air convection turns out to be 891 joules per hour.
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Now our problem wants all these values in watts.
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Watts is a measure of joules per second.
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So we're going to need to convert that 891 joules per hour into joules per second.
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The way we do that is multiply 891 joules per hour by one hour over 3 ,600 seconds, which is how many seconds there are in one hour.
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Now we can cancel out the hours, and we find that the heat from air convection is valued at 0 .2.
05:02
2475 watts.
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So that's the answer to that source of heat.
05:16
Now for solar radiation, all we need to do to find the rate at which the sun heats up the person's skin is take the energy from the sun per meters squared incident on the person's skin.
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This is also known as the solar constant.
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1 ,400 watts per meter squared times the area of the person's exposed skin.
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1 .5 meters squared.
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We multiply that out.
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We get a value of 2 ,100 watts for the heat energy coming from the sun.
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Now, the radiant energy from the environment, the heat from that, can be determined using this expression.
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H is equal to a times e, sigma, times t to the 4, minus t sub s to the 4.
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A is the area of the exposed skin, which we know already.
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E is the emissivity of the skin, which is valued to 1, and sigma is the stefan boltzmann constant, which has a value of 5 .67 times 10 to the minus 8 watts per meter squared times kelm.
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To the fourth.
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Notice that in the denominator of this expression, we have kelvin's, or the units of temperature.
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So what we're going to need to do, we'll still be using 47 degrees celsius for t and 36 degrees celsius for t sub s, but we're going to need to convert them to kelvin's for using that expression there.
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To do that, all we need to do is is add 273 to both of them.
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So t will become 320 kelvin's, and t sub s will be 36 plus 273 gives us 309 kelvin's.
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So now we can begin to plug everything in to find the heat from environmental radiation on this person's skin.
08:26
It'll be equal to 1 .5 meters squared times one, the emissivity of the person's skin, times the stefan boltzmann constant of 5 .67 times 10 to the minus 8 watts, watts, per meter squared times kelvin's to the fourth times 320 kelvin's to the fourth power, minus 309 kelvin's to the fourth power.
09:17
That works out to give the heat of radiation from the environment a value of 116 .45 watts.
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So now we have the rate of heat from these four different mechanisms.
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And considering the sun heats up the person's skin at a rate of 2100 watts, we can consider this source of heat the most important.
09:56
Now, the second part of this question wants us to determine how much the person must perspire in order to maintain a constant body temperature.
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The way we can figure this out is to know that the heat, absorbed by the skin, q, is equal to the mass of person.
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Inspiration developed by the person times the latent heat l.
10:30
Q, rate of heat absorption, is also equal to the total power of each of these four sources of heat from the previous part of the problem times one hour.
10:54
So we have two expressions for q.
10:58
Let's go ahead and equate them to one another, p total times one hour is equal to ml.
11:16
The thing is, we want to find how much this person must perspire in order to maintain this constant skin temperature...