Playground PoundingLesson Plan
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Overview
In this lesson, students
will learn that soils, plants, and people are closely connected. In particular, soils have structure that can
be broken down if trampled by humans or animals. Students will first view and discuss photographs that show where
soil-compression has occurred. Then,
using soil and sponges, students will observe how soil can be compacted, and
the implications of this compaction on soil structure and function. At the end of the lesson, students will have
a deeper understanding of how people, animals, and plants are all connected
through soils.
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Please see the Earth
Systems Foundations - Plants and Soils, Landscape
Changes, Greenlinks,
and Earth
Systems and Humans module descriptions. |
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Lesson Level |
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Mathematics Connections |
·
Students will use non-standard units to measure
water and soil. |
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Science Connections |
· Students will explore soil structure and soil
composition. · Students
will learn that plants are intimately connected to
soils. · Students will recognize that when feet, hooves,
and tires trample plants,
they also compact the soil. · Students
will learn
that compacted
soil can hold less water. |
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Technology Connections |
·
Students
will view aerial photos and satellite images of paths and
compacted soil. |
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Human Connections |
·
Students explain how humans affect plant and animal life
through soil compaction. |
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Lesson Assessment Tools |
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Assessment
and Standards Table (Word) |
· One sponge
(the larger, the better)
·
Clear plastic
2-liter pop bottle cut in half and filled halfway with lightly packed potting
soil
·
Clear plastic
cups filled halfway with potting soil
Procedure
This
is a two-part lesson to be completed over two or more lesson periods.
The
goal of Part I of this lesson is to elicit students’ existing conceptions about
paths and path-making. Teachers might
begin this assessment by asking students to think about sidewalks – What are they? Why do we have them? From this discussion, the teacher then might
encourage students to think about natural paths in grass, or on the
playground. For example: Has
anyone noticed what the grass looks like between _____ and _____? Have you observed anything like this in
other places? How do you think these
paths were first formed? If nobody used
a path ever again, what do you think would happen to it?
The following paragraph includes some
additional background information you may wish to include in the discussion.
People and animals make travel paths for several reasons. Sometimes a path is first taken through thick vegetation because it is the shortest distance between two points. Soon, however, a path becomes well used because it is the easiest way to travel. There are often no longer any plants growing on it, and so it becomes the preferred way even if it isn’t the shortest distance between two different starting and ending points. It is important to note that paths come in many forms—from small paths made by feet and animal hooves, to larger paths (roads) made by the tires of bicycles, motorcycles, and cars.
Prior to engaging in the following hands-on activity, students should view the Pounding and Paths Photo Essay. This part of the lesson will provide students with specific examples of paths and compressed soil. Students will view photos and images that illustrate what happens when soil gets compressed. Teachers may wish to show and discuss the photos and descriptions to the entire class by projecting the photos on a TV connected to a computer or projected on a screen. With each photo invite students to share their observations, ask their own questions, and make connections between the photos and their own life experience. Some children may also share inferences, predictions and theories about what is happening in the photos. You can also use their emerging theories to set the stage for the experiment that will take place in the next part of the lesson.
Background
Information:
So, why is it that plants no longer grow in
soils that have been repeatedly trodden by humans, animals, or tires? Soils are like sponges in several ways. Healthy soils consist of a combination of
mineral and rock fragments, small animals such as earthworms, living and dead
plant tissues such as roots and decaying leaves, and billions of microscopic
organisms called microbes. These
different materials make a miniature underground scaffolding that creates small
air spaces throughout the soil. When it
rains, these air spaces become filled with water, which can then be used by
plants through their roots. When soil
is repeatedly trampled by people, animals, or tires, its miniature structure
breaks down, limiting the soil’s ability to soak up water and decreasing its
ability to support plant life.
1. Set Up Put the following items in an area where all students may
see:
one sponge
a clear plastic 2-liter pop bottle cut in half and
filled partially with loose potting soil
clear plastic cups filled halfway with potting
soil
a small dish tub
glasses or bottles of water
centimeter cubes for measuring
a magnifying glass (optional)
2. Thinking
about Structure
Using centimeter snap cubes, measure the height of the sponge. Now, press down hard on the sponge and
measure its height again with the cubes.
Release the sponge, and then measure again. (The teacher or a student volunteer should record all
measurements on the board.) Repeat this
procedure with soil in the 2-liter pop bottle (use the same starting height as
the sponge). When pressing on the soil,
you may strike the soil repeatedly to simulate a person or animal walking on
it. Students should measure and record
the height of the compacted soil, hopefully noting in particular that it does
not rebound like the sponge did.
Questions
for discussion:
Why do you think we can squish the soil and the
sponge, but we couldn’t possibly squish a rock? (You may wish to illustrate with a rock.)
What is happening when we squish the sponge and
soil? (The sponge and soil both contain empty space within, whereas the rock
is solid. Hence, the sponge and soil
can be compressed as we squeeze out
the air pockets within.)
What do you think takes up the space before we
squished the sponge and soil? (air)
What happened differently after squishing both the soil and sponge? Do they look the same before and after squishing? (The sponge rebounded to its original shape whereas the soil did not.)
3. Predicting. Prepare several different-sized glasses of
water and display on a desk or table.
Ask the students to predict which glass(es) of water the sponge will be
able to hold. Pour water onto the
sponge. If it is a large sponge, it may
hold all of the water in all of the glasses.
Ask the students what allows the sponge to hold so much water. (The
water soaks into the spaces created by air holes.)
4. Observing. To help illustrate the importance of the air
pockets in the sponge, the same activity is repeated, only this time students
try to pour water into a sponge that has been squished. Have a student help squish the sponge, and
over a tub, pour water onto the sponge.
Ask the students what they notice.
Why didn’t the sponge hold much water this time? Release the sponge, and pour water into it
again after it has returned to its normal shape. Was the sponge able to hold water again? The teacher may wish to emphasize that the sponge
is able to soak up so much water because it has much air space in it for water
to soak into.
5. Diagramming. On the chalkboard, model how to record
observations with pictures, numbers and words.
Measurement data should be recorded by including pictures of the stack
of measuring cubes, as well as counting and recording the number of
stacked cubes. Your model will help
children record their own observations in the soil experiment that follows.
6. Squishing
the Soil Activity Sheet. Next, the
students will complete a similar experiment using the cups of soil. Each group should get two cups of soil, two
half-cups of water and the Squishing the Soil Activity Sheet. Have students firmly pack the soil in one
of the cups only. Using the cubes,
they should measure the height of each cup of dirt – one squished, one not –
and then predict what will happen as they pour water into each cup of
dirt. Record their measurements and
predictions on the activity sheet.
Finally, after the soil has been firmly compacted, the students may
slowly pour a cup of water into each cup of soil. The cups of water should be equal in volume. The activity will work best if you try it
yourself first so you know how much water it will take to show the difference
between the cups of dirt. The water
should pool on top of the compacted soil.
Students may draw a picture and describe the results of this experiment
on the activity sheet.
1. Starting the assessment. To begin the assessment portion of the lesson, students will return to several of the images in the photo essay. Distribute the Soil Compaction Activity Sheet. Questions accompany each image, and may be discussed and answered by students. Depending on the literacy skills of the students, this assessment activity may be done individually, in pairs, orally or in writing.
Sample
Question Responses:
Photo of Path and Dogs: Students should understand that the dogs
created that path by walking over it many times. This caused the soil to be squished, which does not allow for
plant (grass) growth.
Photo of Cows: The cows have compacted the soil and eaten
the vegetation.
Wagon Track Photos: Answers will vary. Students should understand that cars compact the soil. Pavement (or concrete) is densely compacted,
solid material. Students may notice
that the plants that now grow on the wagon tracks are significantly different
from those that grow next to the tracks.
Balloon Photo: Students should be able to observe the roads
(paths) made by automobiles.
Satellite Image:
Students should be able to identify the paths in contrast to the existing
foliage captured in the image.
Aerial Photo of Texas: Students should understand that cows walking
along the fences compact the soil along those fences. Students should be able to identify the locations of the fences
by the white lines (cow paths) on the photo.
2. Drawing the soil. As a second assessment task, distribute the Soil Draw Activity
Sheet to students. Students will
complete a diagram of soil that has been compacted by a tractor wheel. Look for students to distinguish between
soil that has and has not been compacted by noting in particular their
illustrations of air pockets in the soil.
3. Assessment
discussion. You might also choose
to lead a whole class discussion about soil compaction to more broadly assess
students’ understandings of the effects of soil compaction on plant growth, and
the ability of underlying soil to hold water and nutrients. The following are ideas for possible
discussion questions.
What are the ways in which paths get made? (Paths
are made because soil has been compressed and plants are unable to grow in
compacted soil. They may be made by
people or animals repeatedly walking over the soil, or by cars, bicycles, or
motorcycles driving over a path.)
Why is it difficult for plants to grow on paths
and roads? (On paths and roads, the soil is compacted and doesn’t allow room for
soil water that nourishes plant roots, and contributes to water running off the
surface instead of infiltrating the soil.)
If you were growing a garden, why would you want
to walk on paths in the garden? (Walking all over the garden would cause
soil compaction where the plants are trying to grow. This would not allow the plants to grow.)
2.
Invite
children to dig up and bring in samples of soil from their yard or
neighborhood. Display the soil and
have kids predict where the soil samples came from. Children might also want to compare the
amounts of water each soil sample can hold.
Photographs used in this lesson were provided
courtesy of Lee Vierling, Steve Archer, NOAA, and the National Park
Service. IKONOS imagery is © Space
Imaging, L.C. and used through the NASA data purchase program.