Cooling Data

Today, we'll be investigating the rate at which boiling water cools in a cup of water

 

First we'll need to examine Newton's Law of Cooling

Newton's Law of Cooling says that the rate of change of the temperature of an object is proportional to the difference between its own temperature and the ambient
temperature (i.e. the temperature of its surroundings).

Newton's Law makes a statement about an instantaneous rate of change of the temperature. The solution to this equation will then be a function that tracks the complete record of the temperature over time.

Newton's Law of Cooling is given by the following:

After some calculus, this yields the following equation:

Where:

 

Table 1. Shows the temperature of boiling water as it cools in a cup of water. The initial temperature is the boiling state at time=0. Each minute (from 0 to 30) the temperature of the water was measured. We have different 31 measurements. Ambient temperature = 71 deg. Initial Temperature of the water =212 deg

Time Temp
0 212
1 207
2 202
3 198
4 194
5 189
6 185
7 180
8 176
9 173
10 169
11 166
12 162
13 159
14 156
15 153
16 151
17 150
18 148
19 146
20 144
21 141
22 140
23 139
24 137
25 135
26 133
27 132
28 131
29 130
30 129

 

Now we use Newton's Law of Cooling to find an equation to model our data. I took time=12 and time = 24 to find k in Newton's Equation. I averaged the two values for k.

 

Table 2 gives us the model temperature, the squared differences between the observed data and the predicted values, and the sum of squares divided by the number of observations

Time Temp Model Temp Model - Obs squared diff
0 212 212 0 0
1 207 207.279767995136 -0.279767995136126 0.0782701311024874
2 202 202.717554360341 -0.717554360341353 0.514884260044888
3 198 198.308069142653 -0.30806914265284 0.0949065966548561
4 194 194.046199479925 -0.0461994799253773 0.00213439194537534
5 189 189.927003672393 -0.927003672393425 0.859335808630897
6 185 185.945705452698 -0.945705452698405 0.894358803263496
7 180 182.097688447738 -2.09768844773754 4.40029682377153
8 176 178.378490825912 -2.37849082591197 5.65721860894739
9 173 174.783800123568 -1.78380012356837 3.18194288084253
10 169 171.309448244635 -2.30944824463458 5.33355119464575
11 166 167.951406627652 -1.95140662765189 3.80798782644373
12 162 164.705781574599 -2.70578157459931 7.32125392944114
13 159 161.568809736094 -2.56880973609429 6.59878346025284
14 156 158.536853747734 -2.53685374773445 6.43562693739435
15 153 155.606398012521 -2.60639801252069 6.79331059967178
16 151 152.774044624471 -1.77404462447137 3.14723432961577
17 150 150.036509428701 -0.03650942870118 0.00133293838408655
18 148 147.390618213396 0.609381786604359 0.371346161845121
19 146 144.833303029267 1.16669697073348 1.36118182151869
20 144 142.36159863222 1.63840136777998 2.6843590419433
21 141 139.972639045113 1.02736095488675 1.05547053162581
22 140 137.663654234612 2.33634576538793 5.45851153544612
23 139 135.431966899297 3.56803310070279 12.7308602077108
24 137 133.274989365294 3.72501063470554 13.8757042286694
25 135 131.190220585829 3.80977941417095 14.5144191846407
26 133 129.175243241226 3.82475675877413 14.6287642637884
27 132 127.227720935992 4.77227906400798 22.7746474647688
28 131 125.345395489732 5.65460451026772 31.97455216754
29 130 123.526084318756 6.47391568124374 41.9115842478536
30 129 121.767677905341 7.23232209465914 52.3064828808948
270.770313259298 sum of squares
8.73452623417091 sum of squares/31

 

 

Using our function we predict the temperature after 45 minutes, 60 minutes, or 300 minutes:

45 101.462910376104
60 89.2791285099322
300 71.0051629863876

We see that at time = 300 minutes our water has cooled to the initial room temperature! Sweet!

To refine our model we could calculate new k values use different times. Say when t=10 and t=20 we can compute another Newton's Cooling Equation with the new k value. By comparing the sum of squares (divided by the number of data points) for both our models, we can see which one is a better fit! A better fit is determined by a lower sum of squares.

 

References:

www.ugrad.math.ubc.ca/coursedoc/math100/notes/diffeqs/cool.html

Sarah Ledford, University of Georgia, Department of Mathematics Education

 

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