Lecture 16 Flashcards

1
Q

Groundwater layers

A
  • unconfined aquifers
  • impermeable rock (aquiclude)
  • confined aquifer
  • impermeable rock (aquiclude)
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2
Q

Aquifers

A

-porous rock units that have enough permeability to supply water at a rate useful to humans

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3
Q

Aquiclude

A

A unit with permeability low enough to form a barrier to flow

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4
Q

Unconfined aquifer

A
  • has a water table everywhere

- upper surface of aquifer is water table

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5
Q

Confined aquifer

A

Bounded above by an aquiclude

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6
Q

Wells in unconfined aquifers

A

-if rate of withdrawal (pumping) exceeds rate of local groundwater flow, can get cone of depression in the water table surrounding the well

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7
Q

Wells in confined (artesian) aquifers

A
  • water table only in recharge area
  • water within aquifer is under pressure
  • water level in lower well rises due to hydraulic head
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8
Q

Solution and mineral precipitation from groundwater

A
  • solution by groundwater
  • caves, sinkholes, and karst
  • deposition from groundwater
    - stalagmites, stalactites
    - cement
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9
Q

Solution by groundwater

A
  • depends on water chemistry, especially pH, groundwater may dissolve minerals
  • CO2 dissolved in rain water makes it slightly acidic
  • calcite (main constituent of limestone) is particularly soluble in acidic water
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10
Q

Caves, sinkholes, and karst

A
  • groundwater solution creates distinctive landscape features in limestone and other soluble rock types
  • caves are very large pore spaces formed by solution
  • sinkholes form where the roof of a cave collapses
  • karst is characterized by numerous sinkholes and/or pillars of rock isolated by solution
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11
Q

Deposition from groundwater

A

-dissolved mineral ions may be deposited in response to:

  1. Evaporation of groundwater in caves
  2. Other changes in chemistry
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12
Q

Stalagmites, stalactites

A
  • mineral deposits (typically calcite) form in air filled portions of caves
  • stalactites resemble icicles hanging from ceiling
  • stalagmites are corresponding pillars growing from cave floor
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13
Q

Cement

A
  • more abundant than stalagmites and stalactites
  • are mineral deposited in small pore spaces
  • cement may convert:
  1. Loose hand into hard sandstone
  2. An aquifer into an aquiclude
  3. A potential oil reservoir into a non porous non reservoir

Huge economic significance

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14
Q

Overland flow and stream flow

A
  • rainfall and melt-water flow down slope under gravity
  • initial sheet-like overland flow
  • erosion creates channels in which flow is concentrated
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15
Q

Stream flow

A
  • base flow (fed by groundwater)
    • no base flow=ephemeral
    • with base flow=perennial
  • storm flow (overland flow into channel from precipitation)
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16
Q

Characteristics of stream systems

A
  • streams are organized in river systems
  • small streams (tributaries) typically merge downstream
  • area drained by a major river and its tributaries is a drainage basin
  • drainage basins are separated by drainage divides