Workshop links
WORKSHOP HOME PAGE
WORKSHOP PRODUCTS
HOLMES
HOME PAGE
MIES HOME PAGE
UTC HOME PAGE
UTC GEOLOGY PROGRAM
Selected links for K-12 Earth sciences
education
AGI's Earthcomm
Enchanted
Learning
Exploring the
Environment
GSA Education
Resources
i4c
Earth Science links
i4c
Elem Earth Sci links
Learning From
the Fossil Record
NASA Athena
NAGT (Geosci. Teachers)
NASTA (Science Teachers)
NCGS
Proj. Earth Sci.
NESTA (Earth Sci. Teachers)
NOVA Teachers
SEPM K-12 Education
TEST
(TN Earth Sci. Teachers)
The WebQuest Page
USGS
The Learning Web
Other useful links
Center for Earthquake
Research and Information (CERI)
Global Volcanism
Program
Hamilton Co. Dept. Ed.
Making of America
Digital library, old works
National Earthquake
Information Center (NEIC)
National Geographic.com
Paleogeography
(Blakely)
Paleomap Project
(Scotese)
Scientific American.com
Univ. Texas map
library
USGS CVO (Cascades)
USGS volcano hazards
VolcanoWorld
Yannarthusbertrand
Photos, Earth from above
Miscellaneous

See the lava lamp
movie
|
|
To return to the page on the groundwater-flow model,
click
here. |
|
For this experiment, 3 wells were fastened to the inside of
the front Plexiglas sheet using silicone sealant. This was done
before the model was assembled.
The wells are lengths of vinyl tubing with open ends. Filter
material was inserted into the lower end of each tube to prevent
sand from entering the wells.
|
 |
|
The "T" in the discharge tube was raised to its
upper limit, such that the model filled with water. The water
supply was then turned off. With the horizontal water table that
soon became established, there is no hydraulic gradient and no
horizontal flow of water through the model.
Red food coloring was added to the 2 outer wells.
This is the initial state of the model for this experiment.
|
 |
|
Water was drawn from the center well using a basting bulb.
Immediately after drawing the water, drawdown was observed in
the 2 outer wells. During drawdown, red dye issued from the bottoms
of the 2 outer wells and migrated toward the center well. Migration
of the dye was driven by the horizontal gradients toward the
center well.
For the duration of the experiment, water was drawn from the
center well every few minutes.
|
 |
|
At 6 minutes, the dye had migrated nearly half way to the
center well.
At 10 minutes into the experiment, the dye had migrated most
of the way to the center well.
Photos for t=6 minutes and t=10 minutes were taken shortly
after drawing water from the center well. Note the drawdown in
the 2 outer wells.
|
 |
| At 18 minutes into the experiment, the dye had
reached the center well. |
 |
| At 25 minutes into the experiment, the dye had
invaded (contaminated) the center well. |
 |
|
At 27 minutes into the experiment, the concentration of dye
in the center well was nearly the same as that of the 2 outer
wells, as judged by the coloration.
Note that photos for t=18, 25, and 27 minutes were taken after
drawdown had recovered.
|
 |
|