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Activity: How Full is Full?
Pre-Req Knowledge (Return to Contents) Some knowledge of multiplication and division is needed. Learning Objectives (Return to Contents) After this activity, students should be able to:
Materials List (Return to Contents) Each group will need:
Introduction/Motivation (Return to Contents) Show the students a cup full of soil. Do you think we could add anything else to the cup? The answer is yes, we could. There is actually space between each of the grains that is filled with air; these spaces are called pores. We could add water to the soil to fill in the pores. Essentially, this is what happens when it rains. Have you ever noticed the difference between really dry soil on a hot day and the same soil after it has rained? What is the soil like when it is wet? (Answer: soggy, damp, etc.) Does the soil take up more space? No, because the water flows through the pores of the soil. How do you think you could measure the volume of the pores in the soil? (Most students will think of pouring water into the cup and measuring how much water fits into the cup.) The ratio of the volume of pores to the total volume the soil fills (pores plus soil grains) is called the porosity. Permeability is the measurement of how easily water flows through soil and is related to the porosity.
Engineers need to find the porosity and permeability of a soil to know where to place a well for bringing up groundwater from an aquifer for drinking water. They also need to develop technologies for drinking water systems to filter harmful germs and chemical spills. Even though a harmful spill may not occur right over a drinking water source, porosity and permeability allows the contaminants to travel through various soils into an aquifer. Today, we are going to try and find the porosity and permeability of different soil samples and use this information to understand groundwater flow. Procedure (Return to Contents) Before the Activity
Note: This lab is written both as an inquiry-based project and a traditional procedures-led lab. Instructions for both methods are provided below. With the Students
To complete activity as an inquiry-based project:
To complete the activity as a traditional lab:
A. Measuring Porosity of Samples
B. Measuring Permeability of Samples
Safety Issues (Return to Contents) Students should follow classroom lab rules at all times. Students should wear safety goggles. Troubleshooting Tips (Return to Contents) If holes get clogged by sand, students can use a pencil to unclog the holes. If water flows through cups too fast, have students repeat and pay more attention to start time. (Note: students may be able to avoid problem if holes are made in advance with the tip of a pencil.) If water takes too long to flow through the hole, have students use exactly half as much water. Assessment (Return to Contents) Pre-Activity Assessment Question/Answer: Lead a general discussion of porosity, permeability and groundwater. Ask students the following questions:
Activity Embedded Assessment Question/Answer: Ask students questions and have them raise their hands to respond. Write answers on the board and discuss as a class.
Porosity and Permeability Worksheet: Have students record measurements in their Data Table and follow along with the activity on their worksheet. After students have finished their worksheet, have them compare answers with their peers. Review their answers to gauge their mastery of the subject. Post-Activity Assessment Prediction Analysis: Have students compare their initial predictions with their test results, as recorded on their worksheet. Ask the students to explain why some soils had a better permeability to water than others. Problem Solving: As an environmental engineer, which of the following soils would you recommend as the best for placing a drinking water well? (Answer: Soil #3, since it has the highest porosity and fastest permeability. Water flows through soils with high porosity more easily.)
Drawing and Class Discussion: Have students depict their subject area knowledge gained by sketching and labeling some of the concepts or activities. For example,
Activity Extensions (Return to Contents) Have students time how long it takes to fill a gallon jug with a water tap on low then calculate the flow rate. (Note: flow rate equals volume; i.e., 1 gallon divided by time in seconds). Then calculate flow rate of a water tap on high. Have students sample the soil from around your school and calculate the porosity of the soil. Have students research the groundwater in your area. Activity Scaling (Return to Contents) For younger students (4th through 6th grade), provide detailed oral instruction for the experiment procedure and possibly just have students calculate porosity. For 7th and 8th grade students, do activity as is. References (Return to Contents) State of Maine, Department of Conservation, Maine Geological Survey, "Ground Water, Wells and the Summer of 1999," http://www.maine.gov/doc/nrimc/mgs/explore/hazards/drought/oct99.htm - accessed October 19, 2005. U.S. Department of the Interior, USGS, Water Science for Schools, Earth's Water: Groundwater http://ga.water.usgs.gov/edu/earthgw.html - accessed October 20, 2005. Contributors Malinda Schaefer Zarske, Janet Yowell, Melissa StratenCopyright © 2005 by Regents of the University of ColoradoThe contents of this digital library curriculum were developed under a grant from the Fund for the Improvement of Postsecondary Education (FIPSE), U.S. Department of Education and National Science Foundation GK-12 grant no. 0226322. However, these contents do not necessarily represent the policies of the Department of Education or National Science Foundation, and you should not assume endorsement by the federal government. Supporting Program (Return to Contents) Integrated Teaching and Learning Program, College of Engineering, University of Colorado at BoulderLast Modified: September 26, 2008
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