EOSC 110 Lecture 13: Streams and Rivers
• HydrologicCycle
• HowstreamsmodifytheEarth'ssurface
HydrologicCycle
•WaterCycleSongVideo
•TheWaterCycleRap(withlyrics)
• Waterisconstantlyonthemove
○ Evaporatedfromoceans,lakes,streams,surfaceoftheland
○ Evaporatedfromplants(transpiraon)bysolarenergy
○ Movedthroughatmospherebywinds
○ Condensestoformcloudsofwaterdropletsoricecrystals
○ Comesbackdownasrainorsnow
○ Flowsthroughstreams,intolakesandeventuallybackintooceans
○ Wateronthesurfaceandinstreamsandlakesinfiltratesthegroundtobecomegroundwater
• Groundwaterslowlymovesthroughtherockandsurficialmaterials
• Somegroundwaterreturnstootherstreamsandlakeswhilesomegoesdirectlybackinto
oceans
RockCycle:
• Weathering,erosionandtransportofmaterialfromthemountainstotheocean‐‐>recyclingof
mineralsintonewrocks
WhyStreamProcessesAreSoImportant
• Streamserode,transportanddepositsediment‐‐>thisformslandscapes
(topography)
• Providemuchofthewaterthatisessenaltoourexistence
• Streamsdowork,dependingon:
○Discharge:Q(cmsorm3/s)
○Velocity:V(m/s)
•Q=VxA
HowDoStreamsErode?
• Dissoluon
• HydraulicFaulng
• Abrasion
HowDoStreamsTransportMaterial?
1. DissolvedLoad
○ Represents,onaverage,about15%ofthemassofmaterialtransported
○ IncludesionssuchasCalciumandChlorideinsoluon
2. SuspendedLoad
○ Thefasterthewaterisflowing,thelargertheparclesthatcanbekeptinsuspensionand
transportedwithintheflowingwater
3. BedLoad
○ Largeparclesrestontheboom
○ Mayonlybemovedduringrapidflowsunderfloodcondions
HowDoStreamsGetEnergy?
• Streamsgetenergyfromslopeanddischarge
• A=graded(equilibrium)streamprofile+baselevel
○ Streamgradient(m/kmor/mile)variesalongprofile
VariaoninStreamVelocity
• Maximumvelocitynearoutsideedgeofmeanders
• Inmeanderingstreams,erosion=deposion
Streams and Rivers
Wednesday,November2,2016 10:54PM