Flowing Water Sediment Transport and Landforms Mediumterm Plan
- Slides: 42
Flowing Water: Sediment Transport and Landforms
Medium-term Plan 10/27 Lecture 13. The Sediment Factory: Source to Sink 11/01 11/03 11/08 11/10 11/15 11/17 11/22 Lecture 14. Flowing Water: Sediment Transport and Landforms Lecture 15. Depositional Systems(HW #4 assigned) Lecture 16. Dating the Sedimentary Record (Thompson) (HW #4 due) Lecture 17. Ice Age Cycles (Thompson) (HW #5? ) Lecture 18: Waves and Coastal Morphodynamics Lecture 19: Shorelines (HW #6 assigned) The Anthropocene: Humans as Geomorphic Agents
Reynolds number (laminar vs. turbulent flow) • u=flow velocity; l=characteristic length (flow depth); =kinematic viscosity (dynamic viscosity/fluid density) (water ~ 1. 5 x 10 -6 m 2/s) • Turbulence is promoted by high flow velocities and flow depths, and low viscosities (Re>2000); laminar flow occurs at Re<500 • Air and water are nearly always turbulent
River Transport of sediment depends upon
Settling Velocity and Cohesion Play bdld. mov
Rivers: Sediment transport • Three modes: • Dissolved load/wash load (ions in solution - pollution) • Suspended load – Fine particles (sand, silt & clay) – Turbulent eddies pick up, carry upward if vel. > settling vel. • Bedload – On/near bed; rolling, bouncing (‘saltating’), etc. • Suspended and bedload increase rapidly with flow strength (nonlinear relationship)
Rivers: Two main kinds • Alluvial rivers; bed consists of sediment (‘alluvium’ = river-associated sediment) – Downstream reaches • Bedrock rivers; part of the bed is bare rock, where river cutting down – generally in upper reaches of rivers
Bedrock Rivers • Erosion rate depends on slope • Presence of sediment (‘tools’) increases erosion
Alluvial Rivers Photo by Duncan Heron
Landform: Floodplain
Landform: Floodplain
Braided stream
• Braided streams are bedload dominated • Nonlinear sediment transport laws result in dynamic feedbacks
Meandering stream; Point Bar and Cut Bank
Point Bars and Cutbanks along river meanders Santee River, SC Photo by Duncan Heron
Neuse River, NC Note point bars Photo by Duncan Heron
Oxbow lake formation Play meander. mov, sm 1. mov
Incised Meanders
Natural Levee formation
Photo by Duncan Heron
Artificial Levees
Levee Failures
Crevasse Splay Deposits, Mississippi River
Natural River - 1948
1964
Drainage Basins
Graded Stream Profile • Flow increases downstream (tributaries) • Velocity Increases • Equilibrium slope reduces as flow increases
Graded Stream Profile • Each stretch of alluvial river tends to have slope adjusted to transport sediment delivered to it • Slope too low, sediment piles up at upstream end -> slope increases • Slope too high, erosion (less in than out) at upstream end -> slope decreases • Need steeper slope with • Less flow • Larger grains
Base Level Changes
Dam cuts off sediment flux
Shelf Transport System
Gravity Flows • Debris flows have a high (>50%) proportion of sediment to water and can be both subaerial and subaqueous • Can occur on land or underwater (Pratson. mov) • Turbidity currents have a higher proportion of water, are always subaqueous, and move due to density contrasts
Pore Pressure • Debris flows have a high (>50%) proportion of sediment to water and can be both subaerial and subaqueous
Pore Pressure • Debris flows have a high (>50%) proportion of sediment to water and can be both subaerial and subaqueous • Terrestrial flows: initial sediment packing affects type of flow Pratson. mov Pdfmod (weak debris flow) Pdfst 6. mov (Strong debris flow)
Gravity Flows • Debris flows have a high (>50%) proportion of sediment to water and can be both subaerial and subaqueous • Can occur on land or underwater (Pratson. mov) • Turbidity currents have a higher proportion of water, are always subaqueous, and move due to density contrasts • The presence of a dilute suspension of sediment in the water of a turbidity current renders it slightly heavier than the ambient water. • This results in downslope movement of both the sediment and entrained water (or vice versa). • Sediment suspension can be from: • catastrophic event (earthquake) • flow-generated turbulence (autosuspension). • wave stirring
Turbidity Currents turbwg. mov (turbidity current) Undf. mov (unconfined tc)
Turbidity Currents • Turbidity currents also create levees, but can overtop them frequently
TURBIDITY CURRENTS – constructional and erosional
Passive (NJ/NY) Shelf
Monterey Submarine Canyon
- Water and water and water water
- Coawst
- Oceaness
- Hydropower from flowing water
- Water flowing downslope along earth's surface
- Force of moving water
- Force of flowing water
- The term geologists use for underground water is
- Water flowing
- Water flowing
- Types of landforms
- Landforms and bodies of water flocabulary answer key
- Natural resources from landforms
- Primary vs secondary active transport
- Primary vs secondary active transport
- Active transport image
- Mesa geology
- Now answer the following questions
- Active transport vs passive transport venn diagram
- Unlike passive transport, active transport requires
- Primary active transport vs secondary active transport
- Bioflix activity membrane transport active transport
- Bioflix activity membrane transport diffusion
- Sediment sorting
- Type of erosion
- Lithogenous sediment definition
- Longshore currents move sediment as they _____.
- Sediment traps construction
- Lithification
- Christchurch bay case study
- Construction entrance
- Lithogenous sediment definition
- Broad sediment-covered continental shelves
- Urinalysis sediment
- Headward erosion diagram
- Table
- A linear ridge of sediment attached to land
- Siliceous ooze
- Geology of holderness coast
- Sediment
- Sediment
- Nierenversagen
- Infiltration