Laboratory Report: Temperature Measurement and Heat Transfer Abstract The purpose of this report is to discuss an investigation into heat transfer from experimentation and background reading. As a fluid has been tested, there will be a focus on convection, both free and forced (stirring). Convection occurs due to hot fluid rising and cooler denser fluid falling (1). Other thermodynamic principles will also be explored. Two different methods of measuring temperature were used with both found to give similar results once appropriated. In addition, it was found that stirring and insulation both had a positive impact on the rate of heat due to doing work on the fluid and reducing heat dissipation. 2 Contents Abstract ...................................................................................................................................... 2 Introduction ............................................................................................................................... 4 Method ...................................................................................................................................... 5 Data and Discussion ................................................................................................................... 7 Conclusion ................................................................................................................................ 13 References ............................................................................................................................... 14 3 Introduction For the experiment, a thermometer and thermocouple were used to record temperature. Despite the two measuring tools differing, the same underlying relationship should be observed. This is an example of calibration (2) and can be used to increase confidence in data. An analogue thermometer uses the proportional relationship of volume and temperature in a liquid to give a reading. As the temperature increases, the liquid will expand and rise up a narrow tube. The height gained is proportional to the increase in temperature and thus can be used to measure the temperature of a body. A thermocouple probe is a highly responsive (under 0.05s(3)) digital measurement device suitable for temperatures between -270 and 3000oC (4). However, they are susceptible to electrical noise (5, 6). The thermocouple can measure temperature due to three effects: the Seebeck effect (Equation 1), the Peltier effect (Equation 2) and the Thomson effect (Equation 3) (7). Although these individual effects will not be further explored in this report, they offer an appreciation for the physical properties which impact the thermocouple’s readings. πΈπππ = −ππ»π Where πΈπππ is the electromotive force (W) π is the Seebeck coefficient (VK-1) π»π is the temperature gradient πΜ = (π±π΄ − π±π΅ )πΌ Where (2) πΜ is the Peltier heat (J) π±π΄ and π±π΅ are the Peltier coefficients (V) πΌ is the electric current between points A and B (A) πΜ = −π π½ ⋅ π»π Where (1) (3) πΜ is heat production rate per unit volume (Wm-3) π is the Thomson coefficient (VK-1) π½ is current density (Am-2) When the beaker is stirred, work will be done on the body of water and this will lead to greater temperature readings (8). This principle is used in industry (9) and thus it is predicted that the rate of temperature increase will increase when the beaker is stirred. In addition, the rate of temperature increase will also increase when the beaker is insulated, as less heat will transfer out of the beaker and be lost to the surrounding air. 4 Method Materials used: Equipment needed: Beaker (1000ml ± 5%) Thermometer (110°C ± 0.5°C) Thermocouple Stopwatch (± 0.01s) Clamp stand Clamp Insulation (sides) Insulation (top) Water Hot plate Magnetic stirred Ruler (1m ± 0.5mm) Figure 1: Equipment Figure 1 shows an image of the equipment required except for the water (which was taken from a laboratory tap), magnetic stirrer and the clamp. Procedure: Firstly, the uninsulated measurements were recorded. The side insulation was not required at this stage. 800ml of water was added to the beaker and the beaker was placed on a flat surface to ensure that the correct amount of water was added - according to the beaker’s calibration line. The thermometer and thermocouple were then placed at the beaker’s lowest line, 20mm upwards from the base. This was achieved by gripping both apparats in the insulation placed on top of the beaker and pushing each measuring device to the bottom of the beaker. An appropriate marking should be made on each measuring device to show the height of each device in relation to the top of the insulation. Using the ruler, a marking 20mm lower can be made which will show the height the device should be at in the beaker. This procedure is partially demonstrated in Figure 2. The hotplate was then heated to 50°C and left for 5 minutes (timed using the stopwatch) to allow the system to stabilise. After, the beaker was placed on the hot plate and the initial temperature was then recorded using both measuring devices. Figure 2: Measuring length methodology 5 Additional readings were taken each minute. The final reading occurred 300s after the initial. After five minutes and six readings, the hot plate was turned off and the beaker removed to avoid unintentional injury from the hot surface. The water was then replaced, and the experiment repeated with the readings now taken from the top of the beaker (80mm), using the same process. Once top and bottom readings had been recorded, the investigation was repeated using a magnetic stirrer at a speed of 300rpm. Top and bottom readings were taken at the same time intervals. Finally, both unstirred and stirred top and bottom measurements were taken when the beaker had the side insulation wrapped around it (shown in Figure 3). All the required raw data had been recorded. Figure 3: Insulated testing 6 Data and Discussion Table 1 contains the raw data readings from the experiment and some basic calculations. The grey cells in the table indicate readings in which the beaker was insulated. Table 1 The ‘TM’ column shows the thermometer readings and the ‘TC’ column shows the thermocouple readings. The corrected thermocouple readings were found by plotting the thermometer’s measurements against the thermocouple measurements and creating a trendline. These values are shown in the ’CTC’ column. The final set of columns presents the mean temperature readings (found using Equation 4) for each set of variables. ππππ = Where ππ + πΆππΆ 2 (4) ππ is the raw thermometer reading (β) πΆππΆ is the corrected thermocouple reading (β) The trendline used to calculate the CTC values is shown in Figure 4. The gradient of this line can be used within Equation 5 to find the corrected values. 7 πΆππΆ = ππΆ + 2.1929 0.9957 (5) ππΆ is the raw thermocouple reading (β) Where It is only possible to correct the thermocouple’s measurements from the more accurate thermometer’s readings (2) due to the linear trend in Figure 4. 29 y = 0,9957x - 2,1929 27 TC /β 25 23 21 19 17 15 15 17 19 21 23 25 27 29 31 TM /β Figure 4: Presentation of proportionality if thermocouple and thermometer readings The horizontal error bars shown in Figure 4 were added due to the ± 0.5β uncertainty in the thermometer’s measurements. As the thermocouple could not be read to a precision greater than 1β, the vertical error bars also have an absolute error of ± 0.5β. As the gradient of Figure 4 is 1.00, once corrected, both pieces of equipment give very similar results. The difference of 2.1929β (shown by the y-intercept in Figure 4) is likely due to the thermocouple originally being mis-calibrated by this amount. Figure 5a and 5b will be used to discuss the impact of stirring. The error bars in these figures were calculated in the same way as those in Figure 4. Figure 5a presents a graph with the mean bottom temperature of the uninsulated tests plotted against time. The trendline of this figure has a gradient equal to the average rate of change of temperature, over time, for the experiment. 8 y = 0,0258x + 19,447 Mean temperature /β 27,0 25,0 23,0 No Stirring y = 0,0077x + 21,141 21,0 Stirring 19,0 17,0 0,0 100,0 200,0 300,0 400,0 Time /s Figure 5a: Comparison of uninsulated mean temperatures when stirred and unstirred The trendline gradients in Figure 5a make it clear that the rate of change of temperature increases drastically when the water is stirred. This is due to the stirrer doing work and giving the individual fluid molecules in the beaker more energy, which in turn vibrates the molecules and increases temperature. As the stirrer is rotating at a constant rate, the amount of work done per unit time is also constant and this leads to a constant relationship represented by the linear trendline. As the hotplate provides constant power, both trends in Figure 5a are linear. The ratio of trendlines in Figure 5a shows that stirring increase the rate of change by 3.35 times. Figure 5b shows the bottom temperature measurements when the beaker was insulated. Mean temperature /β 27,0 y = 0,0231x + 19,591 25,0 23,0 y = 0,0155x + 19,4 No Stirring 21,0 Stirring 19,0 17,0 0,0 100,0 200,0 300,0 400,0 Time /s Figure 5b: Comparison of insulated mean temperatures when stirred and unstirred 9 A sharper gradient (0.0155 compared to 0.0077) indicates that the rate of change approximately doubled when the unstirred vessel had insulation as less thermal energy dissipated to the surroundings. A shallower gradient is observed when comparing the stirred samples however, with the insulated beaker showing a 10% decrease to the gradient in comparison to the uninsulated, stirred sample. Theory dictates that an insulated heated fluid should increase in temperature at a greater rate than an uninsulated beaker (Equation 6, Newton’s Law of Cooling); although one can observe this when comparing the unstirred tests, this is not followed for the stirred. This is likely due to randomised error (e.g. difficulty in reading the thermometer). πΜ ππππ£ = −π΄β(ππ −ππ ) (6) πΜ ππππ£ is the heat transfer rate (W) π΄ is the surface area exposed to the cooling fluid (m2) β is the conventional heat transfer coefficient (W/(m2 K)) ππ is the temperature of the solid body (K) ππ is the temperature of the fluid far away from the solid body (K) Where Data was recorded separately at the top and bottom of the vessel to analyse how the distance from the heat source influences the temperature. Figure 6 presents the difference between top and bottom data readings during stirring. Insulated and uninsulated values have been used. The error bars shown in Figure 6 were calculated in the same way as those in Figure 4. 31,0 Top Temperature /β 29,0 y = 0,8166x + 6,6001 27,0 25,0 23,0 y = 0,8962x + 2,395 21,0 ΠΠΈΠ½Π΅ΠΉΠ½Π°Ρ (Not insulated) ΠΠΈΠ½Π΅ΠΉΠ½Π°Ρ (Insulated) 19,0 17,0 15,0 15,0 20,0 25,0 30,0 Bottom Temperature /β Figure 6: Comparison of top and bottom temperature readings, with and without insulation The top recorded temperature was always greater than the bottom recorded temperature (Figure 6). Although the insulated beaker was cooler than the insulated beaker at all instances, the insulated beaker had a greater rate of temperature increase between bottom and top readings. This is shown by a steeper gradient, 0.8962 compared to 0.8166. The 10 lower readings can be explained due to a lower initial temperature. This could be due to the atmosphere surrounding the apparatus being cooler for the insulated sample than the uninsulated sample. Although the top temperature readings are greater than the bottom temperature readings in absolute terms, it can be inferred that the bottom temperature readings are relatively greater due to the values in gradients for trendlines. Closer to the heat source, heat energy will have less distance to travel and thus will have dissipated less to the surrounding area. The amount of dissipation can be explained by Equation 6 and the side surface area of a cylinder relative to its height (Equation 7), i.e. cooling will increase as surface area increases. π΄π = 2ππ ⋅ π Where (7) π΄π is the side surface area of the cylinder (m2) π is the mathematical constant, pi π is the radius of the cylinder (m) π is the length of the cylinder (m) To estimate the heat transfer rate of the hotplate, the bottom data from when the beaker was both insulated and stirred has been selected. As only work done by the hotplate will be examined, it is unreasonable to use data from the stirred tests. Furthermore, the bottom temperature readings for the insulated test have been chosen to minimise energy loss from dissipation/cooling. The heat transfer rate from the hotplate can be calculated from the total energy change in the volume of water divided by the time the beaker was heated for (300s). The total work done on the beaker of water by the hotplate can be found using Equation 8. π = πππ₯π Where (8) π is energy (J) π is the mass of the fluid (kg) π is the specific heat capacity of the fluid (Jkg-1) π₯π is the change in temperature (K) The specific heat capacity of water is 4186 Jkg-1. The change in temperature may be calculated from the difference between the mean temperature initially and after five minutes. The mean temperature has been chosen to minimise random error by utilising multiple measurements. The temperature difference was found to be 4.5β using this methodology. The mass of the water is calculated using Equation 9. Although density will change with temperature (10), the value will be 1000 kgm-3 to three significant figures (sf) for all initial temperature values used. The volume used is 0.800m3. As the percentage error of the beaker is 5%, this value is accurate to two significant figures. π = ππ (9) 11 Where π is density (kgm-3) π is volume (m3) Therefore, the mass of the water is 0.80 kg. From these values, the work done on the water in total can be calculated as 15100J (3sf). The heat transfer rate can then be calculated using Equation 10, leading to a value of 50.3W for the rate of heat energy transfer from hotplate to water. π= Where π π‘ (10) π is power (W) π‘ is time (s) 12 Conclusion A difference of approximately 2.19β was found between thermometer and thermocouple readings, likely due to the thermocouple being incorrectly calibrated. Due to the highly proportional gradient, it can be assumed both measuring devices are suitable and accurate for temperature measurement. However, there is not complete confidence in this verdict as it is reliant on the assumption that the thermometer used was entirely accurate and precise. Stirring and insulation were both discussed; both had a positive effect on the rate of temperature change with stirring increasing the rate by approximately 3.35 times and insulation doubling the rate. However, as shown in Figure 5b, there is likely to be an error in the results as adding insulation to the stirred sample decreased the rate of temperature change by 10%. Preliminary research suggests this observation to be erroneous and thus the data linking to the observation should be rerecorded. Stating this however, the rest of the data gathered supports current scientific theory and allows this report to achieve its purpose of increasing understanding of heat transfer. The perpendicular distance from a flat heating source was studied by taking measurements at two set distances. In absolute terms, the top temperatures were greater than the bottom temperatures. However, the opposite was true relatively. The relative relationship can be explained by heat travelling a shorter distance and having less availability to dissipate into the surroundings. The absolute difference was possibly due to different atmospheric temperatures causing different initial temperatures. By comparing the trendlines in Figure 6, one notices that gradient is sharper for the insulated sample in comparison to the non-insulated. This is due to the insulation being less thermally conductive than the air and so it is more difficult for heat energy to be lost to the surroundings. An increased understanding into heat transfer has been achieved in this report with strong qualitative comparisons involving insulation and work. Improvements could include using a more precise volume of water to increase confidence in the quantitative result for heat transfer and to ensure a constant ambient temperature – to allow for more reliable comparisons. 13 References 1. Emanuel, K.A. Atmospheric convection. New York;Oxford;: Oxford University Press, 1994. 2. Westwood, A. Lab 1: Temperature Measurement and Heat Transfer [PDF]. Leeds, Faculty of Engineering, 2018 3. Missouri Stante and Technology. Temperature Mesurement [Online] 2000ca [Accessed 20 October 2018]. Available from: https://web.mst.edu/~cottrell/ME240/Resources/Temperature/Temperature.pd f 4. Pollock, D. D. Thermocouples: Theory and Properties. Florida: CRC Press, 1991. 5. Bansel, L. K. et al, Noise Mitigation in Thermocouple Signal Conditioning System for Neutral Beam Calorimeter for NBI SST-1, in IEEE Transactions on Plasma Science. 2014, 42(6), pp.1780-1784 6. Zhang, Z, Liao, X, Wang, X, Research on Thermocouple Distribution for Microwave Power Sensors Based on GaAs MMIC Process, in IEEE Sensors Journal. 2015, 15(8), pp. 4178-4179 7. Beckwith, T.G. and Buck, N.L. Mechanical measurements. [2d]. ed. Reading, Mass U6 - ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi %2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.title=Mechanical+measure ments&rft.au=Beckwith%2C+Thomas+G&rft.au=Buck%2C+Nelson+Lewis&rft.seri es=Addison-Wesley+series+in+mechanics+and+thermodynamics&rft.date=196901-01&rft.pub=AddisonWesley+Pub.+Co&rft.externalDocID=b10444427&paramdict=en-US U7 - Book: Addison-Wesley Pub. Co, 1969. 8. Traynor, C. Stirring Up Trouble. New Scientist. 12 July, 2017 [no pagination] 9. Chen, C., Hu, R. and Luo, X. Experimental and numerical study of a water-stirring radiator. In: 2016: IEEE, pp.610-613. 10. University of Illinois. Density of Wate [Online] 2007 [Accessed 18/10/2019]. Available from: https://van.physics.illinois.edu/qa/listing.php?id=1724 14