Student presentations Flashcards

1
Q

Where was the first comprehensive stormwater and

wastewater system in the country.

A

In Chicago, when the city was raised to make room for the sewers.

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2
Q

What type of plan does TARP utilize?

A

utilizes the “Underflow Plan” - provides greater storage and pumping capacity

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3
Q

What are the 2 phases of the deep tunnel project?

A

○ Phase I - Pollution control, completed in 2006 and in operation
■ Four Tunnels: Mainstream, Des Plaines, Calumet, and Upper Des
Plaines
■ Holds 2.3 billion gallons of volume of combined sewage overflows
○ Phase II - construction of reservoirs, to be complete by 2029
■ Three reservoirs: Gloria Alitto Majewski, McCook, and Thornton
Reservoirs
■ Majewski completed in 1998 - 350 million gallons
■ Thornton completed Sep. 1st, 2015 - 7.9 billion gallons
■ McCook under construction; complete 2029

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4
Q

How many reservoirs will there be for the deep tunnel project?

A

3

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5
Q

3 main aquifer systems in the chicago area

A
  • Sand and gravel deposits from glacial drift
  • Shallow dolomite aquifers of Silurian age
  • Deep sandstone and dolomite aquifers of Cambrian and Ordovician age
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6
Q

Where are the deep paleozoic aquifers?

A

**Paleozoic aquifers in the Chicago region
occur at depths beginning around 500 ft.
and are confined
**Extends through Illinois, Missouri, Iowa,
Minnesota, Wisconsin, Michigan and
Indiana

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7
Q

When did the deep aquifers form?

A

● Paleozoic-542 to 251 Ma

● Cambrian/Ordovician-542 to 445 Ma

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8
Q

What is the deep aquifer system made of?

A

Shale-Aquitard or Seal Rock
Sandstones and Dolomites- Aquifer or Reservoir Rock
Artesian Pressure-Confined aquifer under positive pressure from seal rocks
above and below

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9
Q

Where does water in the deep aquifer come from and go?

A

Recharge:
1. Overlying glacial deposits 47 miles west of Chicago
2. Infiltration through Shale confining layer
Discharge:
1. Human use

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10
Q

What is a glacial aquifer?

A

An aquifer created by glacial action

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11
Q

Features left by glaciation

A
  1. Till
  2. Outwash
  3. Lacustrine Deposits
  4. Sand dunes
  5. Loess
  6. Erratics
  7. Moraines
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12
Q

Major changes to recharge potential caused by human actions

A
  1. Construction of navigable waterways
  2. Diversion of Lake Michigan water
  3. Construction of wastewater treatment plants
  4. Agricultural activities
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13
Q

Flow conditions into bubbly creek

A

very little drainage
stagnant water during dry season
overflow from combined sewers (can get back into other parts of the system)

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14
Q

Sediment quality of bubbly creek

A
  • Heavily influenced by meat processing
  • average thickness about 13 feet
  • biochemical reactions can carry clumps of sediment to the surface
  • not considered hazardous waste
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15
Q

What makes it difficult for plants and wildlife to inhabit bubbly creek?

A

Stagnant conditions, lack of base flow, and continued sewer overflow make it difficult for plants and wildlife to inhabit the creek

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