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Hydrologic cycle
- ocean water evaporates; (liquid) --> (gas)
- condensation; (gas) --> (liquid) or (solid)
- precipitation
- infiltration (groundwater) and runoff (rivers)
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potential energy
energy of position
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adiabatic heating/cooling
- temperature change due to volume change
- ↑volume = ↓temperature
- ↓volume = ↑temperature
- -- no heat exchanged
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aquifer
groundwater reservoir
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permeability
ability to allow the passage of fluids; interconnectedness of pores
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porosity
- the amount of our rocks/sediments that are void space
- expressed as a percentage of total volume
- primary: porosity that forms with rocks/seds deposition
- secondary: forms due to weathering/erosion
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recharge
- the refilling of our groundwater reservoir
- largely due to infiltration
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infiltration
- movement of water through soils and rocks
- manner of transport of precipitation into groundwater system
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anatomy of an aquifer, top to bottom
- surface
- -----------------------------
- zone of aeration (vadose zone)
- -----------------------------
- capillary fringe
- ------------------------water table
- zone of saturation
- __________________
- bedrock or impermeable layer
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three types of aquifers
- unconfined; the upper surface is the water table
- confined; impermeable layers above (aquiclude/aquitard) and below (bedrock)
- perched; a lens of water that gets trapped above an impermeable bit of sed or rock
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potentiometric surface
height to which pressurized water can pump itself using its potential energy
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recharge basin
- collects water in a depression which creates pressure
- uses that pressure to pump water into ground
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anatomy of a river/stream
- headwaters; place water originates
- tributaries; small channels that combine to form larger streams
- trunk, main channel; larger streams
- distributaries; smaller channels form when river chokes itself with sediment
- delta
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gradient
- change in elevation ÷ horizontal distance
- slope
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thalweg
- deepest and highest velocity portion of a channel
- highly erosive part of a river
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bedload
sediment that is rolled or dragged along the bed of a river
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suspended load
seds that are carried in the flow of a river
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dissolved load
ions that are carried in the river water
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discharge (Q)
- the volume of water that flows past a point in a given time
- Q = velocity x area
- or, cubic feet per second
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describe a meandering stream
- the thalweg migrates to the outside of bends in a sinuous channel, creating...
- cutbank; a region of increased erosion on the outside of a bend
- point bar; a region of increased deposition on the inside of a bend
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oxbow lake
an abandoned bend that is cut off from the main channel due to sediment deposition
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characteristics of an urban stream
- infiltration is slowed/stopped due to pavement
- all precipitation will directly enter the channel
- large discharge (tall peak on hydrograph)
- velocity will be high due to rapid input of water
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characteristics of a rural stream
- infiltration forms a lag in the hydrograph
- runoffs begin when the soils become saturated
- runoff is slower due to soils, plants, etc. so the maximum discharge slowly builds and falls
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types of floods
- flash floods
- regional floods
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flash floods
- intense rain over a small area over a short amount of time
- fast moving runoff
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regional floods
- sustained rain over large drainage
- slow rise and fall
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recurrence interval
- amount of time expected to pass between floods of the same size
- RI = (n+1) ÷ m
- n: number of years of data
- m: numerical rank of the flood
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probability that a flood will occur in any given year
p = 1 ÷ RI
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channelization
- if you decrease the roughness in bed, you increase the velocity of flow
- allows for the movement of more water in less time
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anatomy of a beach, top to bottom
- marine terrace
- cliff
- berm
- beach face
- wave-cut platform
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wave-cut platform
flat ledge cut into bedrock due to wave activity
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beach face
portion of beach where sand is transported due to wave activity
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berm
portion of beach above high-tide line where the sand does not move
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marine terrace
elevated wave-cut platform
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wave frequency =
- 1/wavelength
- shorter wavelengths have higher frequency = more energy
- longer wavelengths have lower frequency = less energy
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longshore transport
the transport of sediments along a coast at an angle to the shoreline, which is dependent on prevailing wind direction, swash and backwash
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swash
onshore movement of water in a wave
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backwash
the offshore movement of water in a wave
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4 man-made structures that interfere with sand drift:
- jetties; closely spaced groins designed to keep longshore transport from closing off a waterway
- groins; beach ⊥ structure; designed to slow down the longshore current
- breakwater; beach || structure; built offshore to prevent waves from reaching the shore, forms calm area
- seawall; beach || structure; built on beach, prevents waves from striking the beach
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