Lecture 15 Flashcards

1
Q

Phases of water

A
  • liquid water
  • ice
  • water vapour

Transitions between phases absorb and release energy (latent heat of melting and vaporization)

Absorb energy going from more ordered to less ordered phase

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2
Q

Properties of ice

A
  • unusual mineral
  • polar character
  • open crystal lattice
  • lower density than liquid form
  • water expands as it freezes

Consequences:

  • ice floats
  • expansion of freezing water fractures rocks
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3
Q

Properties of liquid water

A
  • excellent solvent for ionic and polar substances
  • a small portion of water molecules are dissociated into H+ and OH-
  • H+ actually attached to near by water molecule to make a hydronium molecule
  • high surface tension as a result of polarity and H bonding
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4
Q

pH

A

The -log[H+]

Ocean is slightly alkaline whereas surface waters are quite acidic

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5
Q

Hydrologic pathways

A
  • condensation/precipitation
  • evaporation and transpiration
  • infiltration and subsurface flow
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6
Q

Hydrologic reservoirs

A
  • oceans (97.5%)
  • ice sheets (2%)
  • groundwater (0.64%)
  • lakes, rivers, atmosphere (0.01%)
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7
Q

Largest reservoir of fresh water?

A

Polar ice sheets

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8
Q

Largest reservoir of unfrozen fresh water?

A

Groundwater

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9
Q

Hydrologic pathways

A

Condensation:

  • water vapour to liquid or solid
  • falls as precipitation (rain or snow)

Evaporation:
-from sea or land

Transpiration:
-from plants

Surface flow:

  • glaciers (melting)
  • rivers and streams

Subsurface flow:
-infiltrations (groundwater movement)

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10
Q

Hydrologic budget

A

Fluxes:

Greatest for atmosphere then ocean then land

Overall closed system

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11
Q

Groundwater

A
  • groundwater flow
  • water in the lithosphere
  • solution and mineral precipitation from groundwater
  • free water in pore spaces within the solid Earth
  • less then 1% of earth’s water
  • exact amount uncertain, especially at depth
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12
Q

Porosity

A
  • the amount of empty space (pores) in a sediment or rock
  • expressed as % by volume
  • can be filled with air, water, oil, natural gas..
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13
Q

Permeability

A

-measure of the ease through which fluid can flow through a rock

Depends on:

  • porosity
  • size of pore spaces
  • connectedness
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14
Q

Zones of groundwater

A

Zones of aeration: pores partly filled with water

Zones of saturation: pore spaces entirely filled

Water table: the surface separating these zones

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15
Q

Form of the water table

A
  • water table typically rises under hills
  • generally a subdued imitation of shape of landscape
  • rises and falls with variations in rainfall and discharge of water
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16
Q

What drives groundwater flow?

A
  • groundwater flows from regions of high pressure to regions of low pressure
  • at a given depth, pressure is higher if water table is higher
  • hydraulic head measures pressure difference driving flow
17
Q

Recharge and discharge areas

A

Recharge: water passes from surface into groundwater system

Discharge: water exits from groundwater system into surface water