Digital Collections @ Dordt Faculty Work: Comprehensive List 1-7-2017 Weighing Fog: Hands on Modeling for Day 1 of Differential Equations Tom Clark Dordt College, [email protected] Follow this and additional works at: http://digitalcollections.dordt.edu/faculty_work Part of the Mathematics Commons Recommended Citation Clark, Tom, "Weighing Fog: Hands on Modeling for Day 1 of Differential Equations" (2017). Faculty Work: Comprehensive List. 639. http://digitalcollections.dordt.edu/faculty_work/639 This Conference Presentation is brought to you for free and open access by Digital Collections @ Dordt. It has been accepted for inclusion in Faculty Work: Comprehensive List by an authorized administrator of Digital Collections @ Dordt. For more information, please contact [email protected]. Weighing Fog: Hands on Modeling for Day 1 of Differential Equations Abstract The first day of many mathematics classes contains formalities and very little mathematics. Here an alternative is presented where modeling is placed as the centerpiece to orient students to the real work of differential equations. Namely, to capture as beautifully and compactly as possible through the process of conjecture and investigation, the deep and interesting aspects of the physical world. A demonstration of the sublimation of dry ice sits at the center of the lesson. Students collaborate in groups to design an experiment that could measure the change in mass of a piece of dry ice that is dropped into water, the experiment is then carried out, and finally the students (with some guidance) build and solve a model for the phenomenon. I will also present my reflections on the lesson as well as guidance and resources for use in the differential equations classroom. Keywords mathematical models, differential equations, physical science, dry ice Disciplines Mathematics Comments Presented at the 2017 Joint Mathematics Meetings held January 4-7, 2017, in Atlanta, Georgia. This conference presentation is available at Digital Collections @ Dordt: http://digitalcollections.dordt.edu/faculty_work/639 Weighing Fog: Hands on Modeling for Day 1 of Differential Equations Thomas J. Clark January 7, 2017 Dordt College 1 in my beginning is my end The Goal Mathematics begins in wonder and ends in understanding. 3 The Goal Mathematics begins in wonder and ends in understanding. 1. Capture attention of students. 2. Ask interesting questions. 3. Start with modeling, let the differential equations follow from need. 4. Students do the thinking, generate ideas. 5. Let day 1 be a microcosm of the semester. 6. Don’t discuss syllabus on day 1; they can read it, or I can make a screencast and they watch later. 7. The more I think about it, this could probably fill the first two days of class, especially if it is done via IBL. 3 The Question Question What will happen if I drop a piece of dry ice into water? 4 The Question Question What will happen if I drop a piece of dry ice into water? Question (Follow Up) What is the graph of the mass over time? How do you find the equation of that function? 4 5 The Outline 1. Pose dry ice question. 6 The Outline 1. Pose dry ice question. 2. Students design experiment that could measure mass of dry ice over time. 6 The Outline 1. Pose dry ice question. 2. Students design experiment that could measure mass of dry ice over time. 3. Run experiment (just borrow the scale and dry ice from the chemistry department). 6 The Outline 1. Pose dry ice question. 2. Students design experiment that could measure mass of dry ice over time. 3. Run experiment (just borrow the scale and dry ice from the chemistry department). 4. Make conjectures about mass/time function. 6 The Outline 1. Pose dry ice question. 2. Students design experiment that could measure mass of dry ice over time. 3. Run experiment (just borrow the scale and dry ice from the chemistry department). 4. Make conjectures about mass/time function. 5. Model with differential equations. Discuss what a mathematical model is. 6 The Outline 1. Pose dry ice question. 2. Students design experiment that could measure mass of dry ice over time. 3. Run experiment (just borrow the scale and dry ice from the chemistry department). 4. Make conjectures about mass/time function. 5. Model with differential equations. Discuss what a mathematical model is. 6. Compare “solution” to data, revise/improve model. 6 The Model 7 The Model 1. Students suggest “exponential decay”. 8 The Model 1. Students suggest “exponential decay”. 2. Clarify to y (t) = Ce kt . 8 The Model 1. Students suggest “exponential decay”. 2. Clarify to y (t) = Ce kt . 3. Move to y 0 = ky , what this means...change in mass is proportional to mass. Does that seem right? 8 The Model 1. Students suggest “exponential decay”. 2. Clarify to y (t) = Ce kt . 3. Move to y 0 = ky , what this means...change in mass is proportional to mass. Does that seem right? 8 The Model: Take 2 1. How does the dry ice sublimate? Where? 9 The Model: Take 2 1. How does the dry ice sublimate? Where? On the surface. 9 The Model: Take 2 1. How does the dry ice sublimate? Where? On the surface. 2. So y 0 = k · Surface Area. 9 The Model: Take 2 1. How does the dry ice sublimate? Where? On the surface. 2. So y 0 = k · Surface Area. 3. What is mass proportional to? 9 The Model: Take 2 1. How does the dry ice sublimate? Where? On the surface. 2. So y 0 = k · Surface Area. 3. What is mass proportional to? Volume. 9 The Model: Take 2 1. 2. 3. 4. How does the dry ice sublimate? Where? On the surface. So y 0 = k · Surface Area. What is mass proportional to? Volume. How do you relate volume and surface area for a cube? 9 The Model: Take 2 1. 2. 3. 4. 5. How does the dry ice sublimate? Where? On the surface. So y 0 = k · Surface Area. What is mass proportional to? Volume. How do you relate volume and surface area for a cube? Propose y 0 = ky 2/3 . But what is the solution? 9 The Model: Take 2 1. 2. 3. 4. 5. How does the dry ice sublimate? Where? On the surface. So y 0 = k · Surface Area. What is mass proportional to? Volume. How do you relate volume and surface area for a cube? Propose y 0 = ky 2/3 . But what is the solution? 9 The Extensions 1. Vary mass to surface area ratio: y 0 = ky r . dy = kdt yr 1 y 1−r = kt + C 1−r 1 y (t) = (1 − r )(kt + C ) 1−r . 10 The Extensions 1. Vary mass to surface area ratio: y 0 = ky r . 2. Assume k = k(t), changes with time. (Plot ‘k(t)‘ = y 0 /y 2/3 ) 10 The Extensions 1. Vary mass to surface area ratio: y 0 = ky r . 2. Assume k = k(t), changes with time. (Plot ‘k(t)‘ = y 0 /y 2/3 ) 3. Attempt to model water mass loss from “fog”. 10 The Resources Worksheet: http://homepages.dordt.edu/~tclark/DryIce/DryIce.pdf Run 1: 4.4 grams of dry ice sublimating: https://youtu.be/1qyiyBRpj-8 Run 1: Screen capture of mass/time data: https://youtu.be/_4DhfnH02a8 Run 2: 11.42 grams of dry ice sublimating: https://youtu.be/EogDv4yXBJA Run 2: Screen capture of mass/time data: https://youtu.be/Xa9wmxzgxGM 11 the end of all our travels Thanks For Your Attention! If you would like to see any of my materials contact me at [email protected]. References 1. Clark, Thomas J, “Weighing Fog: Modeling on Day 1 of Differential Equations,” (pre-print). 2. Winkel, Brian (2015), “1-12-T-SublimationCarbonDioxide,” https://simiode.org/resources/435. 13
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