Experiment 1
Did Mr. Plover bury the crowbar?

 

crowbarExperiment 1
In this experiment we will discover whether or not the crowbar from the scene of the crime was buried by a snodlop (most likely Mr. Plover) or buried under sediment deposited from the the Stumporl Stream.

 

I] Hypothesis
Soil from shoveling dirt into a hole will look different than soil deposited in a hole from moving water, such as a stream.

 

II] Materials needed

• two clear 2-liter soda bottles or 2 large glass jars with lids.
• a large spoon or small shovel
• a bucket or pale to collect the dirt
• magnifying glass
• a permanent marker
• a funnel or rolled piece of paper (you will only need this of you are using the 2-liter soda bottles.)

 

III] Procedure

 

  1. Read through all the steps of the procedure before starting your experiment.
  2. Collect enough soil to fill at least one 2-liter soda bottle. Make sure your soil sample is made up of different size particles. Best to collect your soil sample from three different areas; making sure each area consists of different size particles from the previous area.
  3. Using a spoon, small shovel or stick mix your soil sample thoroughly.
  4. If you are using 2-liter soda pop bottles cut one of the bottles in half and discard its top in a recycling bin. Mark the lower half “shovel” with a permanent marker. If you are using large glass jars mark one of the jars “shovel”. Mark your other container“stream”.jars
  5. Using a spoon or small shovel fill the container you marked “shovel” with soil from the sample so it is about 10 centimeters (~4 inches) deep and set it aside.jar or plastic
  6. Using a spoon or small shovel fill the container you marked “stream” with soil from the sample so it is about 4 inches deep. If you are using a 2-liter soda bottle you may need a funnel or rolled piece of paper to get the soil into the bottle without spilling.
  7. Fill the rest of the container marked “stream” with water. Leave about 3 centimeters (just over an inch) of space at the top of the container so you won’t spill the water.Fill Line
  8. Cap the container marked “stream” securely and shake thoroughly until all the soil is caught up in the swirling water. This represents sediment suspended in the moving water of the stream.
  9. Set the well shook container down next to the container marked “shovel” and let it rest overnight.
  10. The next day, using your magnifying glass look carefully at the two soil samples. What do you observe?Sediment Grain Size
Loading experiment form.
Coming Soon
Which picture of the soil above best matches your sample labeled SHOVEL?
Loading experiment form.
Coming Soon
Which picture of the soil above best matches your sample labeled STREAM?
IV] Detective Conclusions:
Now that you have conducted the experiment, entered your experimental results, and reviewed what other detectives observed you should be able to better deduce the character of Mr. Plover. Does knowing if Mr. Plover was telling the truth help you in determining who stole the key?
V] Further Exploration
The water velocity of a river changes as it meanders through the countryside. River bends, as well as width and depth greatly affect water speed. What type of sediment would  you expect to find in shallow parts of the river where the river is moving slowly compared to deeper areas where the water is more rapidly.  Next time you visit a river or stream look carefully at the inside and the outside of a bend in a river. Do you notice any difference in the sediment of these two parts of the river.
VI] Relating to the Environment

The river bed of a fast-flowing stream usually is made up of heavier gravel and stones because all the lighter soils are carried away. River deltas have very fertile ground because the water slows as it branches out, depositing lighter, organic particles that are nutrient rich.

The damming of rivers for irrigation and other industry has the disadvantage of preventing the natural fertilization of the land from periodically flooding.

Creek bed

Snicktaw Creek
Note: That large rocks and pebbles along the shore were deposited in the spring, after a seasonal snow melt, when the water level was higher and moving more rapidly.