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  • Tips & Modifications

    Tip

    To save students' data for grading online, register your class for free at the High-Adventure Science portal page.

    Tip

    This activity is part of a sequence of activities in the lesson Will There Be Enough Fresh Water?. The activities work best if used in sequence.

    Modification

    This activity may be used individually or in groups of two or three students, or as a whole class activity. If using as a whole class activity, use an LCD projector or interactive whiteboard to project the activity. 

    1. Engage students in thinking about how water moves through sediments.

    Tell students that much of their water comes from groundwater and that water moves from the ground to the surface. Ask:

    • Why does water move through gravel more quickly than it moves through clay? (Gravel is more permeable than clay.)
    • Would it be easier to get water out of sand or out of gravel? (It would be easier to get water out of gravel because the pore spaces are larger. The water will move more quickly through larger pore spaces.)

     

    2. Discuss the role of uncertainty in the scientific process.

    Tell students that science is a process of learning how the world works and that scientists do not know the “right” answers when they start to investigate a question. We can see examples of scientists' uncertainty in the forecasting of precipitation amounts. Have students go to NOAA National Weather Service. Ask them to input their zip codes, hit “Go”, scroll down to the bottom of the page, and click on the “Hourly Weather Graph”. This page shows the hourly weather forecast for your area. The first box shows the predicted temperature and dew point (along with wind chill or heat index, when applicable). The second box shows the predicted wind speed and direction. The third box shows the predicted sky cover (i.e. cloud cover), relative humidity, and chance for precipitation. The boxes below that line show whether the precipitation is likely to be rain, snow, freezing rain, or sleet. Point out the line for precipitation potential (the brown line). Ask:

    • Why is the precipitation shown as a “%”? (Precipitation is dependent on other factors, such as relative humidity and temperature. It is more likely to precipitate when the temperature is the same as or lower than the dew point.)
    • If there is a likelihood of precipitation, why is the amount of rain/snow shown as ranges? (The amount of precipitation that will fall is dependent on the amount of moisture in the atmosphere. The atmosphere is continually changing, so the amounts are guidelines for what could happen rather than perfect predictions.) 

      *If there is no or low likelihood of precipitation in your area, you may want to find a different location (in the United States) that has a higher likelihood of precipitation. You can look at a current weather map (radar) to find where in the United States precipitation is happening currently. Your students will then be able to see scientists' forecasts of precipitation amounts represented as a range overlaid on the bar graphs.

     

    Tell students they will be asked questions about the certainty of their predictions and that they should think about what scientific data are available as they assess their certainty with their answers. Encourage students to discuss the scientific evidence with each other to better assess their level of certainty with their predictions.


    3. Introduce the concept of systems in Earth's water resources.

    Tell students that forecasting what will happen to Earth's fresh water supplies is a complicated process because there are many different interacting parts. Tell students that scientists think about how one part of the system can affect other parts of the system. Give students a simple example of a system, as described in the scenario below.

     

    On an island, there is a population of foxes and a population of rabbits. The foxes prey on the rabbits. Ask: 

    • When there are a lot of rabbits, what will happen to the fox population? (It will increase because there is an ample food supply.) 
    • What happens to the fox population when they’ve eaten most of the rabbits? (The foxes will die of starvation as their food supply decreases.) 
    • What happens to the amount of grass when the fox population is high? (The amount of grass will increase because there are fewer rabbits to eat the grass.)
    • If there is a drought and the grass doesn’t grow well, what will happen to the populations of foxes and rabbits? (The rabbit population will decrease because they have a lesser food supply. The fox population should also decrease as their food supply decreases.)

    Humans introduce dogs to the island. The dogs compete with the foxes over the rabbit food supply. Ask: What will happen to the populations of foxes, rabbits, and grass after the dogs are introduced? (The foxes will decrease because they are sharing their food supply, the rabbits will decrease because they have more predators, and the grass will do well because of the lowered impact of the smaller rabbit population.)

     

    Tell students that simple cause-effect relationships can expand into more complex system relationships. Let students know that they will be exploring the relationship between how sediments and rock types affects groundwater movement. Encourage students to think about how human actions play a role in changes in the flow of water and in freshwater availability.

     

    4. Introduce and discuss the use of computational models.

    Introduce the concept of computational models, and give students an example of a computational model that they may have seen, such as forecasting the weather. The weather forecast provides a good example of how model input is used to predict future conditions. Go to NOAA Weather Forecast Model. Tell students that scientists used current information about the energy and moisture in the atmosphere as an input to the model, and that what they see on the weather map is the output of the model's calculations.


    5. Have students launch the Groundwater and Surface Water interactive.

    Provide students with the link to the Groundwater and Surface Water interactive. Divide students into groups of two or three, with two being the ideal grouping for sharing computer workstations. Inform students they will be working through a series of pages of models with questions related to the models. Ask students to work through the activity in their groups, discussing and responding to questions as they go.

     

    NOTE: You can access the Answer Key for students' questions—and save students' data for online grading—through a free registration on the High-Adventure Science portal page.

     

    Let students know that this is Activity 4 of the Will There Be Enough Fresh Water? lesson.


    6. Discuss the issues.

    After students have completed the activity, bring the groups back together and lead a discussion focusing on these questions:

    • How does the water table affect the relative amount of water in surface bodies and underground? (When the water table is high, meaning the soil is saturated, water will move [or stay] above ground and surface bodies of water will expand. When the water table is low, water will move from the surface downward toward the ground.)
    • What are the effects on a stream of removing too much water from the ground? (If too much water is removed from the ground, the stream can dry up. The water table can be lowered below the level of the stream.)
    • How can humans better manage their use of limited water supplies? (Humans can conserve water. They can use the wastewater to recharge the water supplies.)
    • Are rivers an endless supply of fresh water? (Rivers are not an endless supply of fresh water. They can be run dry if the water table goes too low. This can happen when people withdraw too much water from the river and/or from the groundwater that supplies the river. Even though the rivers still receive precipitation, they can be depleted if the water table isn't high enough.)

     

    Informal Assessment

    1. Check students' comprehension by asking students the following questions:

    • How does water move between groundwater and surface water when the water table is high?
    • What can humans do to keep water flowing in streams?

    2. Use the answer key to check students' answers on embedded assessments.

  • Subjects & Disciplines

    • Science
      • Earth science
      • General science

    Learning Objectives

    Students will:

    • describe how water moves between the ground and surface water bodies depending on the level of the water table
    • describe the effects on a stream of withdrawing too much water

    Teaching Approach

    • Learning-for-use

    Teaching Methods

    • Discussions
    • Multimedia instruction
    • Self-paced learning
    • Visual instruction
    • Writing

    Skills Summary

    This activity targets the following skills:


    Connections to National Standards, Principles, and Practices

    National Science Education Standards

    Common Core State Standards for English Language Arts & Literacy

    ISTE Standards for Students (ISTE Standards*S)

    • Standard 3:  Research and Information Fluency
    • Standard 4:  Critical Thinking, Problem Solving, and Decision Making

    Next Generation Science Standards

  • What You’ll Need

    Required Technology

    • Internet Access: Required
    • Tech Setup: 1 computer per learner, 1 computer per pair, Interactive whiteboard, Projector

    Physical Space

    • Classroom
    • Computer lab
    • Media Center/Library

    Grouping

    • Heterogeneous grouping
    • Homogeneous grouping
    • Large-group instruction
    • Small-group instruction
  • Background Information

    Water moves between the groundwater and surface bodies of water. Gaining streams gain water from the groundwater. Losing streams lose their water to the groundwater. The level of the water table determines which way water will move between the groundwater and surface. Humans can alter the water table by withdrawing water from the groundwater with wells.


    Prior Knowledge

    • None

    Vocabulary

    Term Part of Speech Definition Encyclopedic Entry
    aquifer Noun

    an underground layer of rock or earth which holds groundwater.

    Encyclopedic Entry: aquifer
    confined aquifer Noun

    layer of water-bearing rock between two layers of less permeable rock.

    conservation Noun

    management of a natural resource to prevent exploitation, destruction, or neglect.

    Encyclopedic Entry: conservation
    freshwater Noun

    water that is not salty.

    groundwater Noun

    water found in an aquifer.

    Encyclopedic Entry: groundwater
    model, computational Noun

    a mathematical model that requires extensive computational resources to study the behavior of a complex system by computer simulation.

    permeable Adjective

    allowing liquid and gases to pass through.

    porosity Noun

    the ratio of the volume of all the pores, or holes, in an object and the object's total mass.

    porous Adjective

    full of tiny holes, or able to be permeated by water.

    precipitation Noun

    all forms in which water falls to Earth from the atmosphere.

    Encyclopedic Entry: precipitation
    recharge Verb

    to renew or restore to a previous condition.

    runoff Noun

    overflow of fluid from a farm or industrial factory.

    Encyclopedic Entry: runoff
    stream Noun

    body of flowing water.

    Encyclopedic Entry: stream
    sustainability Noun

    use of resources in such a manner that they will never be exhausted.

    system Noun

    collection of items or organisms that are linked and related, functioning as a whole.

    topography Noun

    the shape of the surface features of an area.

    unconfined aquifer Noun

    layer of water-bearing rock covered by permeable rock.

    water cycle Noun

    movement of water between atmosphere, land, and ocean.

    Encyclopedic Entry: water cycle
    water table Noun

    underground area where the Earth's surface is saturated with water. Also called water level.

    Encyclopedic Entry: water table

    Reference

Partner

Funder

National Science Foundation - HAS

This material is based upon work supported by the National Science Foundation under Grant No. DRL-1220756. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.