Lecture 15 Flashcards
Phases of water
- 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
Properties of ice
- 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
Properties of liquid water
- 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
pH
The -log[H+]
Ocean is slightly alkaline whereas surface waters are quite acidic
Hydrologic pathways
- condensation/precipitation
- evaporation and transpiration
- infiltration and subsurface flow
Hydrologic reservoirs
- oceans (97.5%)
- ice sheets (2%)
- groundwater (0.64%)
- lakes, rivers, atmosphere (0.01%)
Largest reservoir of fresh water?
Polar ice sheets
Largest reservoir of unfrozen fresh water?
Groundwater
Hydrologic pathways
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)
Hydrologic budget
Fluxes:
Greatest for atmosphere then ocean then land
Overall closed system
Groundwater
- 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
Porosity
- the amount of empty space (pores) in a sediment or rock
- expressed as % by volume
- can be filled with air, water, oil, natural gas..
Permeability
-measure of the ease through which fluid can flow through a rock
Depends on:
- porosity
- size of pore spaces
- connectedness
Zones of groundwater
Zones of aeration: pores partly filled with water
Zones of saturation: pore spaces entirely filled
Water table: the surface separating these zones
Form of the water table
- 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