stream ecology: river structure and hydrology unit 1: module 4, lectures 1
TRANSCRIPT
Stream Ecology: River Structure and Hydrology
Unit 1: Module 4, Lectures 1
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s2
Objectives
Students will able to: describe how evaporation and precipitation
influence river formation. diagram the distribution of water on Earth. define and provide examples of a watershed. diagram stream networks and drainages. explain how a meandering stream can form an
oxbow lake. predict riffle and pool formation in a stream
segment.
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s3
Module 4 introduces students to:
Lecture1: The Importance of
Rivers The Hydrologic Cycle Watersheds as a
concept Geomorphology
watersheds and drainage networks
channel morphology habitat scales
Lecture 2: Hydrology
flow and discharge storm and annual
hydrographs flood probability sediment transport and
deposition
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s4
Rivers: Provide water and nutrients for agriculture Provide habitat to diverse flora and fauna Provide routes for commerce Provide recreation Provide electricity
www.aquatic.uoguelph.ca/rivers/chintro.htm
Importance of rivers
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s5
Existence depends on: Availability of surface water A channel in the ground An inclined surface
www.aquatic.uoguelph.ca/rivers/chintro.htm
Natural watercourses
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s6
Four dimensions: Longitudinal Lateral Vertical Time
Lotic systems
www.aquatic.uoguelph.ca/rivers/chintro.htm
The four dimensions of a lotic system
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s7
The shape, size and content of a river are constantly changing, forming a close and mutual interdependence between the river and the land it traverses.
www.aquatic.uoguelph.ca/rivers/chintro.htm
Variation in time and space
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s8
Effect of climate
Rivers are very dependent on climate and their characteristics are closely related to the precipitation and evaporation regimes in their drainage areas.
Three types: Perennial or permanent rivers Periodic rivers Episodic rivers
www.aquatic.uoguelph.ca/rivers/chintro.htm
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s9
The hydrologic cycle
ga.water.usgs.gov/edu/charts/waterdistribution.gif
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s10
ga.water.usgs.gov/edu/charts/waterdistribution.gif
Distribution of water on earth
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s11
www.dec.state.ny.us/website/2000/watersheds.gif
What is a watershed?
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s12
What is a watershed?
www.aquatic.uoguelph.ca/rivers/chwater.htm
www.dec.state.ny.us/website/2000/watersheds.gif
www.epa.gov/watertrain/ecology/ecology21.html
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s13
Spatial scale: Stream segments
www.usda.gov/stream_restoration/chap1.html
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s14
www.aquatic.uoguelph.ca/rivers/chwater.htm
www.usda.gov/stream_restoration/chap1.html
Stream networks or drainages
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s15
Stream order
A method of classifying or ordering the hierarchy of natural channels.
Strahler (1957) is the most widely used system. Stream order correlates well with drainage
area, but is also regionally controlled by topography & geology.
www.usda.gov/stream_restoration/chap1.html
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s16
Spatial scale: Segment system
www.usda.gov/stream_restoration/chap1.html
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s17
http://www.usda.gov/stream_restoration/Images/scrhimage/chap1/fig1-15.jpg
Stream corridor and channel morphology
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s18
www.usda.gov/stream_restoration/chap1.html
Cross section of a channel
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s19
Floodplain
www.usda.gov/stream_restoration/chap1.htmlFigure 1.21
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s20
Meandering rivers
http://www.aquatic.uoguelph.ca/rivers/chphys.htm
A meander becomes more pronounced as the streamline shifts between the river banks.
Formation of an oxbow lake
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s21
Small meanders high gradient coarse substrates
Sinuosity: Gradient and substrate
Big meanders low gradient fine substrates
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s22
Braided Pattern = high slope + high stream power + coarse bed materials
Braided channel
earthsci.org/teacher/basicgeol/stream/stream.html#Erosion%20by%20Streams
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s23
dnr.metrokc.gov/WTD/wetland79/images/oxbow-01-30.jpg
An oxbow lake
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s24
Spatial scale: Reach system
www.usda.gov/stream_restoration/chap1.html
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s25
Riffles, pools, and cascades
Riffles and pools alternate in somewhat predictable patterns
www.aquatic.uoguelph.ca/rivers/chphys.htm
Developed by: Merrick, Richards Updated: August 2003 U1-m4-s26
Pool - riffle sequence
Riffle to riffle = 5 - 7 channel widths
http://www.usda.gov/stream_restoration/Images/scrhimage/chap1/fig1-15.jpg