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Analysis of Groundwater Seepage at Hansom Landfill: Slug Test Data and Linear Regression, Study Guides, Projects, Research of Introduction to Business Management

Data from slug tests conducted at three wells located at the hansom landfill site. The data is used to determine the rate of groundwater seepage into the rock surrounding the reservoir, also known as the permeability of the rock. Instructions for performing a linear regression analysis on the data to find the best fit line and determine the slope and y-intercept.

Typology: Study Guides, Projects, Research

Pre 2010

Uploaded on 08/05/2009

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Project Grant Team
John S. Pazdar Patricia L. Hirschy
Project Director Principal Investigator
Capital Comm-Tech College Asnuntuck Comm-Tech College
Hartford, Connecticut Enfield, Connecticut
This project was supported, in part, by the Peter A. Wursthorn
National Science Foundation Principal Investigator
Opinions expressed are those of the authors Capital Comm-Tech College
and not necessarily those of the Foundation Hartford, Connecticut
NASA - AMATYC - NSF
5.17
SPINOFFS
Spinoffs are relatively short learning modules inspired by the LTAs. They can be easily
implemented to support student learning in courses ranging from prealgebra through calculus.
The Spinoffs typically give students an opportunity to use mathematics in a real world context.
LTA - SPINOFF 5A Functional Risk Assessment
LTA - SPINOFF 5B Slugging It Out
LTA - SPINOFF 5C Calculating the Reference Dose
LTA - SPINOFF 5D Using the World Wide Web to Do Risk Assessment
LuAnn Malik - AMATYC Writing Team Member
Community College Of Aurora, Aurora, Colorado
(Currently at Community College of Arapahoe, Colorado)
Pete Wildman - AMATYC Writing Team Member
Casper College, Casper, Wyoming
Joe Voor - NASA Scientist/Engineer
Kennedy Space Center, Florida
(Currently at The Johnson Space Center, Houston, Texas.)
pf3

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Project Grant Team

John S. Pazdar Patricia L. Hirschy Project Director Principal Investigator Capital Comm-Tech College Asnuntuck Comm-Tech College Hartford, Connecticut Enfield, Connecticut

This project was supported, in part, by the Peter A. Wursthorn National Science Foundation Principal Investigator Opinions expressed are those of the authors Capital Comm-Tech College and not necessarily those of the Foundation Hartford, Connecticut

NASA - AMATYC - NSF

SPINOFFS

Spinoffs are relatively short learning modules inspired by the LTAs. They can be easily implemented to support student learning in courses ranging from prealgebra through calculus. The Spinoffs typically give students an opportunity to use mathematics in a real world context.

LTA - SPINOFF 5A Functional Risk Assessment

LTA - SPINOFF 5B Slugging It Out

LTA - SPINOFF 5C Calculating the Reference Dose

LTA - SPINOFF 5D Using the World Wide Web to Do Risk Assessment

LuAnn Malik - AMATYC Writing Team Member Community College Of Aurora, Aurora, Colorado (Currently at Community College of Arapahoe, Colorado)

Pete Wildman - AMATYC Writing Team Member Casper College, Casper, Wyoming

Joe Voor - NASA Scientist/Engineer Kennedy Space Center, Florida (Currently at The Johnson Space Center, Houston, Texas.)

NASA - AMATYC - NSF

SPINOFF 5B

Slugging It Out

You did such an excellent job on the first problem as a risk assessor that your skill is greatly admired throughout NASA. Because of your talents and skills, you are selected to do some additional analysis of the Hansom Landfill Site. Here is a more detailed description of the site:

The Hansom Dam Landfill is located approximately one mile south of the Visitor’s Center on the southern side of Ransom Road, one mile west of the intersection of Ransom Road and Kennedy Parkway South. The site is bordered to the north by Ransom Road, to the east by a General Services Administration storage yard, and to the west and south by a wetland that flows into the Indian River. Directly west of the site is a drainage trench, which eventually flows into the Indian River. Underneath the soil at the landfill is a reservoir of groundwater.

Hazardous waste deposited at a landfill can result in the potential for pollution of groundwater under the landfill. When it rains on the landfill, water flows through the landfill site and could eventually end up in the groundwater below the landfill. As the water flows through the landfill, it will pick up any soluble chemical compounds in the landfill and carry these chemicals into the groundwater. If this process is continued over a long period of time, it can create serious contamination of the groundwater. The Hansom Landfill is over 30 years old, and therefore the potential for significant contamination exists. The landfill site is closed to the public. However, since the groundwater eventually seeps into the Indian River, the presence of contaminants could have an effect on industrial workers, residents and recreators.

NASA has ordered a series of tests to determine the rate at which the groundwater seeps into the river water. The type of test ordered is called a slug test. This is how a slug test works. A hole is dug into the ground until groundwater is reached. A tube is inserted into the hole, and into the tube is inserted a piece of lead called a slug. As the slug is lowered into the groundwater, the level of the groundwater will rise. This process is called displacement. It is the same process that occurs when you drop a small rock into a can of water – the water will rise after the rock is dropped into it. However, unlike the can of water, the rock surrounding the groundwater reservoir is not watertight! The rock will allow some of the groundwater to seep into it. This is of concern, since eventually this groundwater may make its way to other water sources used by humans. If the groundwater in the reservoir is contaminated, this could present a potential health hazard to anyone using these other sources of water. When the slug is dropped into the water, initially the water will rise to a high level. However as the water seeps into the rock surrounding the reservoir, the level of the water will fall over time. You are concerned with the rate at which the water seeps into the rock surrounding the reservoir. This rate is referred to as the permeability of the rock.