Measuring Streams Flashcards
First order steams: (2)
No branching.
Smallest stream sections.
It takes two streams of the
Same order to raise to the next stream order downstream.
Second order streams are a
Combination of two first order streams.
Third order streams are
A combination of two second order streams.
Law of stream numbers: higher order streams in a basin are
Less abundant than lower order streams. The decrease in abundance occurs in a regular fashion.
Law of stream numbers: The bifurcation ratio (Rb) is the
Ratio between the number of stream segments in one order and the next.
Law of stream numbers: Bifurcation ratio -
Generally between 3 and 5.
Nu = Rb ^(k-u)
k - highest stream order.
u - stream order
Law of stream numbers:
Bifurcation ratio (Rb) =
Nu / Nu+1
Nu - number of streams in given order.
Nu+1 - number of streams in next highest order.
Law of stream lengths: High order streams are
Longer; the length increases in a regular way.
Law of stream lengths:
Length ratio (RL) =
Lu / Lu-1
Lu - mean length of streams in order u
Lu-1 - next lowest order.
Law of drainage density: A measure of
The length of the stream channel per unit area of the drainage basin.
Law of drainage density:
```
Drainage density (Dd) =
Km km-2
~~~
Σ(Nu x Lu) / Ab
Nu x Lu) - Total stream length (km
Ab - Basin area (km2)