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Underground Water Flow and Darcy's Law

Difficulty
Time Required Average (6-10 days)
Prerequisites None
Material Availability Readily available
Cost Low ($20 - $50)
Safety No issues

Abstract

This project shows you how to build a simple model system to simulate underground water flow. Underground water flow is important for understanding replenishment of underground aquifers, migration of underground contaminant plumes, and cave formation. With your model system, you can simulate various underground conditions, and test your predictions about the effects they have on water flow.

Objective

The goal of this project is to model the flow of groundwater, and to calculate the flow rate using Darcy's formula.

Credits

Andrew Olson, Ph.D., Science Buddies

Sources

This project is based on:

Cite This Page

MLA Style

Science Buddies Staff. "Underground Water Flow and Darcy's Law" Science Buddies. Science Buddies, 27 Sep. 2013. Web. 27 Aug. 2014 <http://www.sciencebuddies.org/science-fair-projects/project_ideas/Geo_p014.shtml>

APA Style

Science Buddies Staff. (2013, September 27). Underground Water Flow and Darcy's Law. Retrieved August 27, 2014 from http://www.sciencebuddies.org/science-fair-projects/project_ideas/Geo_p014.shtml

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Last edit date: 2013-09-27

Introduction

Fresh water exists not only in lakes and streams on the surface of the earth, but also underground. These subsurface sources of freshwater are called underground aquifers, and the water in them is called groundwater.

Like water on the surface, groundwater can also flow. And like water on the surface, groundwater also flows downhill. Groundwater can also move in response to differences in pressure from the overlying rock, soil, and water. The rate of groundwater flow will also depend on the material through which the water is flowing. Materials that are more solid will reduce the flow rate, while materials that are more porous will increase the flow rate.

Darcy's Law is a relationship that explains fluid flow in porous media, such as often seen in geological formations. The basic formula to calculate the flow rate, Q, is:

Q = KA (h1 − h2) / L

where:
  • K is a permeability coefficient (describes the porosity of the underground formation),
  • A is the cross sectional area,
  • h1 is the height of the inlet head,
  • h2 is the height of the outlet head, and
  • L is the path length of the flow.

Understanding how groundwater moves is important for predicting how quickly underground aquifers will be replenished when water is drawn up from wells drilled down from the surface. Sometimes groundwater can become tainted with salt water or even toxic compounds seeping from a contaminated source. In these cases it is especially important to understand groundwater movement, in order to contain the spread and prevent contamination of aquifers used for drinking water or irrigation.

In this project, you will use plastic soda bottles to make models of water flowing through underground formations. You will fill the bottles with different materials (e.g., sand, gravel, silty clay, etc.) and then measure water flow to see the effects of different types of formations. You can investigate the effects of pressure by making outlets at different heights on the bottle. The height of the water above the outlet creates the pressure, so the lower the outlet is, the more pressure there will be. By measuring the flow rate at the outlet, you can see how well Darcy's Law predicts your results.

Terms and Concepts

To do this project, you should do research that enables you to understand the following terms and concepts:

  • groundwater,
  • aquifer,
  • porosity,
  • Darcy's Law,
  • artesian well,
  • drawdown.

Bibliography

These websites will help you get started with your background research on groundwater and Darcy's Law:

Materials and Equipment

To do this experiment you will need the following materials and equipment:

  • 4 (or more) 2 L plastic bottles,
  • plastic tubing (e.g., aquarium tubing, drinking straw). Plastic tubing may be available locally from aquarium or hardware shops or online from suppliers such as Carolina Biological, catalog #671784.
  • sharp knife,
  • modeling clay,
  • graduated beaker for measuring outflow. A 400 ml glass beaker is available from Carolina Biological, catalog #721210. Alternatively, a large, graduated measuring cup may be used.
  • timer or stopwatch,
  • material to simulate subsurface, e.g.:
    • pea gravel,
    • aquarium gravel,
    • sand,
    • clay soil,
    • mixtures of clay and sand.

Disclaimer: Science Buddies occasionally provides information (such as part numbers, supplier names, and supplier weblinks) to assist our users in locating specialty items for individual projects. The information is provided solely as a convenience to our users. We do our best to make sure that part numbers and descriptions are accurate when first listed. However, since part numbers do change as items are obsoleted or improved, please send us an email if you run across any parts that are no longer available. We also do our best to make sure that any listed supplier provides prompt, courteous service. Science Buddies does participate in affiliate programs with Amazon.comsciencebuddies, Carolina Biological, and AquaPhoenix Education. Proceeds from the affiliate programs help support Science Buddies, a 501( c ) 3 public charity. If you have any comments (positive or negative) related to purchases you've made for science fair projects from recommendations on our site, please let us know. Write to us at scibuddy@sciencebuddies.org.

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Experimental Procedure

  1. Do your background research and make sure that you are knowledgeable about the terms, concepts, and questions, above.
  2. Prepare at least four 2 L bottles for measuring flow rates, as described in Figure 1, below:
    2 L soda bottle with outlet holes
    Figure 1. Each soda bottle should have a single outlet hole. Make four bottles, each with an outlet hole at a different height. To collect the outflow, connect a short length of drinking straw or aquarium tubing to the outlet hole, and seal the edges with modeling clay. Use a large measuring cup or other graduated container to catch the outflow. (Thanks to John LeVasseur for the soda bottle drawing from which this diagram was adapted.)

  3. To investigate the effect of pressure on underground water flow, compare the flow rate from the different outlet holes. Fill each bottle with the same medium (e.g., sand).
    • Keep the water level in the bottle constant by pouring water in at the top.
    • Measure the outflow by collecting the water in a graduated container and measuring how much water you collect in a given time period (e.g., 10, 20, or 30 seconds).
    • Convert your flow rate to liters per minute for comparing the different conditions.
    • Calculate the pressure head for each condition by measuring the difference between the heights of the inlet (h1) and outlet (h2). The arrows in Figure 2 show the pressure head (h1 − h2) for each of the outlet holes.
    • Graph your results by plotting flow rate (y-axis) vs. delta h (the inlet height minus the outlet height, as shown in Figure 1). How well does Darcy's Law predict your results?
  4. To investigate the effect of different materials on underground water flow, use different materials to fill the bottles. Compare the measured flow rates for the different materials (using outlets at the same height). Can you use Darcy's Law to calculate the K value (permeability coefficient) for each material?

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Variations

  • What do you think will happen to flow rate if you change the diameter of the bottle? Can you relate this change to groundwater movement?
  • What do you think will happen to the flow rate if you change the diameter of the outlet tubing?

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Ask an Expert

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