| Lesson Plans:
How Fast Do Sediment Grains of Different Sizes Settle?
Students will define rate, turbidity, and settling rate and explain
the relation between settling rate and turbidity.
Students will interpret change in turbidity with time as a function
of settling rates of sediment of different grain sizes.
Students will predict how the clarity of water in a stream or in the
ocean will differ during periods of flood vs. low water, or during a
storm vs. between storms, and explain the basis for this prediction.
What Goes on Down Under?
Students will explain the sources for recharge and discharge of
groundwater, identify the connection between surface and
groundwater, and describe the relationship between soil grain size
and water flow rate.
Particle Size Demonstration
Demonstrations in Soil Science
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