# QR Teaching Activities

# Show all Resources

# Subject

- Biology 12 matches
- Chemistry 8 matches
- Economics 3 matches
- Education 1 match
- Engineering 2 matches
- Environmental Science 13 matches
- Geography 1 match
- Geoscience 31 matches
- Health Sciences 1 match human health topics
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- Mathematics 15 matches
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# Quantitative Skills Show all Quantitative Skills

- Exponential Growth and Decay 18 matches
- Logarithms 30 matches

## Logarithms/Exponential Functions

19 matches General/OtherResults 1 - 10 of **54 matches**

Kohler Curves part of Quantitative Skills:Activity Collection

Swarndeep Gill, California University of Pennsylvania

An assignment teaching students about Kohler curves that enhances their quantitative skills.

Two streams, two stories... How Humans Alter Floods and Streams part of Quantitative Skills:Activity Collection

Eric Baer, Highline Community College

An activity/lab where students determine the changes in 100-year flood determinations for 2 streams over time.

Understanding Radioactivity in Geology: The Basics of Decay part of Quantitative Skills:Activity Collection

Christina Stringer—University of South Florida, Tampa FL 33620
This activity was developed for Spreadsheets Across the Curriculum . National Science Foundation, DUE 0442629.

PowerPoint module leading students through creation and manipulation of spreadsheet to forward model an example of exponential decay—the number of remaining unpopped kernels of popcorn in a bag of popping popcorn.

Estimating Exchange Rates of Water in Embayments using Simple Budget Equations. part of Quantitative Skills:Activity Collection

Keith Sverdrup, University of Wisconsin-Milwaukee

Simple budgets may be used to estimate the exchange of water in embayments that capitalize on the concept of steady state and conservation principals. This is especially true for bays that experience a significant exchange of freshwater. This exchange of freshwater may reduce the average salt concentration in the bay compared to seawater if it involves addition of freshwater from rivers, R, and/or precipitation, P. Alternatively, it may increase the average salt concentration in the bay compared to seawater if there is relatively little river input and high evaporation, E. Since freshwater input changes the salt concentration in the bay, and salt is a conservative material, it is possible to combine two steady state budgets for a bay, one for salt and one for water, to solve for the magnitude of the water flows that enter and exit the bay mouth. Students will make actual calculations for the inflow and outflow of water to Puget Sound, Washington and the Mediterranean Sea and compare them to actual measured values.

Radiocarbon dating project part of Cutting Edge:Topics:Rates and Time:Teaching Activities

Mark Schmitz, Boise State University

This is an example of an activity used in a Quaternary Geochronology course, in which a small group of students (3-4) is tasked with transforming a set of activity measurements into radiocarbon ages and calibrated ...

What is the Volume of the 1992 Eruption of Cerro Negro Volcano, Nicaragua? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor, University of South Florida-St. Petersburg

SSAC Physical Volcanology module. Students build a spreadsheet to calculate the volume a tephra deposit using an exponential-thinning model.

What is the Relationship between Lava Flow Length and Effusion Rate at Mt Etna? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor, University of South Florida-St. Petersburg

SSAC Physical Volcanology module. Students use Excel to determine a log-log relationship for flow length vs effusion rate and compare it with a theoretical expression for the maximum flow length.

How Do We Estimate Magma Viscosity? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor, University of South Florida-St. Petersburg

SSAC Physical Volcanology module. Students build a spreadsheet to examine how magma viscosity varies with temperature, fraction of crystals, and water content using the non-Arrhenian VFT model.

Math Review part of Cutting Edge:Courses:Hydrogeology:Hydrogeology, Soils, Geochemistry 2013:Activities

Kallina Dunkle, Austin Peay State University

This is designed as an introductory lab for hydrogeology or other upper-level courses that are quantitative in nature in order to review key mathematical concepts that will be used throughout the semester.

Viscosity of the Mantle: Constraints from Post-glacial Rebound part of Quantitative Skills:Activity Collection

David Kohlstedt, University of Minnesota

This laboratory experiment emphasizes the exponential nature of post-glacial rebound and reinforces the relationship between the rate of rebound and the viscosity of the mantle.