Geography/Geology 352: Geomorphology

STREAM SEDIMENT

Picture (650x10, 1.6Kb)

 

A. Introductionphoto: sandy/gravelly river bar

1. Types of energy: potential, kinetic, thermal

2. Entrainment: set of processes that initiate particle motion

3. Thresholds: under what conditions will a river do the mechanical work necessary to modify or maintain channel morphology?

4. Agenda:


B. Hydraulic Factors Affecting Entrainment

hjulstrom diagram1. Critical bed velocity

a. sixth power law: r3 = kv6

b. Hjulstrom diagram

2. Critical bed shear stress

a. shear stress

b. bed shear stress

tb = r x g x r x s = g x r x s

where: r = density of water

g = gravity

r = hydraulic radius

s = slope

g = unit specific weight of water

c. Shields diagram

shields diagram

3. Velocity gradientdiagram: lift force

a. rate of change in velocity with distance from bed or banks

b. velocity gradient creates a vertical pressure gradient, which results in an upwards force

c. velocity gradient steeper for turbulent flow than for laminar flow

d. for a given discharge and area:

4. Stream power: w

w = r g Q s / w

where: r = density of water

Q = discharge

s = slope

w = channel width


C. Sediment Characteristics Affecting Entrainmentphoto: cutbank sediment layers

1. Size and density

2. Sorting of bed material

3. Layering or packing

4. Particle shape and orientation

photo: river bank vegetationD. Bank Erosion

1. Fluvial entrainment: corrasion

2. Weakening and weathering processes

a. reduce strength of bank material

b. soil moisture condition is most important control


E. Transportation
photo: muddy braided river

1. Suspended load

2. Bed load offsite link icon: bed load movie

3. Dissolved load

F. Deposition

1. Ripples offsite link icon: ripple migration movie

2. Dunes

3. Antidunes offsite link icon: antidune movie


G. Summary

1. mechanical work: erosion, transportation & deposition

2. type of work function of:

3. amount of work

© K.A. Lemke (klemke@uwsp.edu)
Last modified January 15, 2007