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Demystifying the Equations of Sedimentary Geology Larry Lemke Environmental Science Program Department of Geology
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GOALS Alleviate student apprehensions –Build confidence –Establish effective habits Refresh and review –Reinforce key concepts –Connections with math, physics, and chemistry
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Presentation Format Goals and Objectives Three approaches I use –Surgical strike reviews –Unit analyses –Perturbation interrogation Discussion: Dealing with Student Math-a-phobia –Strategies –Experiences
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1. Surgical Strike Reviews Explain what you’re doing and why you’re doing it Use at the beginning of class Keep it brief – 10 minutes tops! Stay focused – only target what you’ll actually use in the day’s lecture. Revisit in subsequent lectures 5 to 10-minute review of relevant math principles targeted for a specific lecture What:
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2. Unit Analysis Use routinely after presenting or deriving a new equation. Use common units to move toward generic (Mass, Length, Time) units: Assigning fundamental units of Mass, Length, and Time to analyze an equation What:
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Unit Analysis Apply to derived quantities or units, such as centipoises for dynamic viscosity: Assigning fundamental units of Mass, Length, and Time to analyze an equation What:
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3. Perturbation Interrogation Use in combination with Unit Analysis. Use with simple quantities: F=ma Works great with ratios: How does an equation change when its individual components increase or decrease? What:
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3. Perturbation Interrogation One More Example Engelund & Hansen nondimensional sediment flux Express coefficients as constants Shields parameter or “Sheilds Stress” “What does this equation tell me?”
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3. Perturbation Interrogation One More Example Shear stress – proportional to water depth (h) and stream gradient (S) Substituting into canceling
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3. Perturbation Interrogation One More Example Substituting into: Will sediment flux increase or decrease if… …the water depth (h) increases? …the stream gradient (S) increases? …the grain diameter (D) increases?
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Discussion Your experiences Your solutions
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