Fluvial Geomorphology 2 Flashcards
even though average velocity is relatively lower at headwaters, ___ velocity can be very high. Why?
instantaneous
b/c there is lots of up & down (pools and riffles on the bed)
If slope/ gradient were the only factor, velocity would ___ downstream, but because channel roughness, wetted perimeter ratio, and discharge all change downstream too, velocity actually ___ as you go downstream
decrease
actually increases
why does discharge increase downstream?
Because tributaries combine= increases the volume of water flowing through the channel = higher discharge
as area increases, ___ water is in contact with the bed (ie. ____ and ____)- deeper/shallower, wider/ narrower
This means ___ friction and therefore ___ velocity
less
deeper & narrower
less
higher
What is the range of manning’s roughness coefficient (n)?
0.01 to 0.05
(smooth to rough)
Reynolds number=
measure of flow turbulence (internal friction in the fluid column due to flow destruction)
more turbid= bigger or smaller range of instantaneous velocities?
more turbid= bigger range
higher bed loads typically= ___ (wider or narrower) channels
wider
b/c harder to move
which is easier to measure, bedload or suspended load?
suspended load
bed load hard to measure because it happens very episodically (high velocities are needed)
dissolved load relates to rate of ___ weathering
chemical
When might chemical weathering be high?
ie high dissolved load
high temp, high rainfall, high groundwater flow inputs
t/f
fine clays can be classified as dissolved load
true!
They’re sometimes small enough that they’re classified as ‘dissolved’
sediment yield=
amount of sediment transported by a river relative to its upstream basin area
sediment yield ___ with drainage basin size
decreases
b/c dilution?
how do you convert sediment yield to erosion/ denudation rate?
turn tonnes into density
depth/time x 1/rock density