Teacher Site Map
4thGrade Core
USOE Science Home Page
USOE

Sizing It Up!

 
The solid part of soil is made from mineral and organic matter. You know a little bit about organic material. MagnifiedRockNow it is time to learn more about the inorganic parts of soil. Do you remember what other solid materials are in soil? (Hint: You need them to be healthy.) The answer, of course, is minerals. Minerals come from rocks. Minerals become part of the soil in several different ways. Sometimes minerals are added to the soil from volcanic eruptions. Most minerals, however, come from rocks that are broken apart over a very long period of time.  
 
Size wise
Just as daisies, dinosaurs, and doughnuts come in different sizes; so does soil. Soil particles come in different sizes. Scientists group these into three categories: sand, clay, and silt. Sand has the largest particle size. Clay is the smallest size. Guess where silt fits in? If you said in between the two, you are absolutely correct. Here is an example of how to visualize the relationship between sand, silt, and clay. If a particle of sand is a basketball, then silt is the size of a softball, and clay is the size of a golf ball.
 
The size of soil particles is important. Knowing this helps you understand the type of soil that you have in your yard or your garden. The amount of open space between the particles has to do with the ease that water moves through soil and the amount of water the soil holds.
 
The best kind of soil for plants allows water to move easily enough to be absorbed by the root system and slow enough to allow water to stay in the soil for continued use by the plant. A soil with a high percentage of sand allows water to move too quickly. The roots of plants have little time to absorb the moisture. Clay particles are so small; they pack closely together holding water tightly. Plant root systems cannot get to the water. Soils that have the ideal mixture of sand, silt, and clay are the best type of soil for plants. These soils are called loams.
 

Do it!

Use your sense of touch to determine the type of soil you have in your garden. Sand feels gritty. Silt feels smooth, soft and somewhat slick. Clay feels sticky and often leaves a color stain on your fingers. Soils that have a lot of clay can be pressed between thumb and forefinger to create a ribbon of soil.

 

You be the scientist!

Problem: How can you determine the composition of the soil in your yard?

 

Materials:

  • 250 - 500 ml (one or two cups) of soil from your yard or garden.
  • One liter (one quart) jar with a tight fitting lid
  • 15 ml (one tablespoon) of a powdered water conditioner such as Calgon®
  • Water
  • Ruler (metric)
 

Procedure:

  1. Place the soil in the jar.
  2. Add the water conditioner.
  3. Fill the jar approximately two thirds full of water.
  4. Place the lid on the jar and secure tightly.
  5. Shake the jar until the ingredients are thoroughly mixed.
  6. Allow the jar to sit undisturbed for about 72 hours.
  7. Carefully bring the jar to your work area.
  8. Observe your soil. If your soil is typical of most soils, you will notice a layering of the soil. These layers are the sand, silt, and clay.
  9. Using a ruler, measure the length (in centimeters) of the three layers from the bottom of the jar to the top of the soil. Do not include the water in your measurement. If you have some other organic material floating at the top, you do not need to measure it.
  10. Record the total volume of the soil in centimeters.
  11. Next, measure and record the total volume of each layer of soil. (You may not have all three layers in your soil sample. If this is the case, compare your soil to a classmate's soil to find out which layer you are missing in your soil sample.)
  12. Ask your teacher or parent to help you determine the percentage of each layer.
  13. Which type of particle will be found at the bottom, middle and top? Why? To find the answer, highlight the box below.
    ANSWER: Because sand is the biggest and heaviest of the three particles, it will sink to the bottom first, so the bottom layer is sand. Silt will be the middle layer. You will find the clay at the top.
  14. Write a summary or draw a picture of your findings. Discuss these findings with your parents. Maybe you can actually do something to make your garden more productive. And that is what science is all about!
  15. Write a summary or draw a picture of your findings. Discuss these findings with your parents. Maybe you can actually do something to make your garden more productive. And that is what science is all about!
 

Analysis:

  1. What kind of soil particle was the most common in your soil sample?
  2. From what kind of rocks do you think your soil was formed?
  3. How did your soil sample compare to the soil samples of your friends?
  4. The ideal soil is called a loam. It is a mixture of 40% sand, 40% silt, and 20% clay. What would have to be done to your soil to make it a loam? HINT: You would have a difficult time taking these tiny particles out of your soil.

 

Download the plug-ins: Get Adobe Acrobat Reader , and Get Quicktime Player. (The QuickTime plug-in is needed to play sounds and movies correctly.)

Want to share photos of you or your friends doing this activity? Send it in an e-mail with the following information:

  1. The title of the activity
  2. The URL (Internet address)
  3. Your name.

Remember that no pictures can be used that show student faces or student names on it. 

Teachers should view the Teacher Site Map to relate Sci-ber text and the USOE 4th grade science core.


Updated October 24, 2008 by: Glen Westbroek

Science Home Page | Curriculum Home Page | 4th Grade Science Core Home Page | USOE Home Page


Copyright © Utah State Office of Education.