stream ecology: river structure and hydrology unit 1: module 4, lectures 1

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Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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Page 1: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Stream Ecology: River Structure and Hydrology

Unit 1: Module 4, Lectures 1

Page 2: 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.

Page 3: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 4: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 5: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 6: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 7: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 8: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 9: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s9

The hydrologic cycle

ga.water.usgs.gov/edu/charts/waterdistribution.gif

Page 10: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s10

ga.water.usgs.gov/edu/charts/waterdistribution.gif

Distribution of water on earth

Page 11: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s11

www.dec.state.ny.us/website/2000/watersheds.gif

What is a watershed?

Page 12: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 13: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s13

Spatial scale: Stream segments

www.usda.gov/stream_restoration/chap1.html

Page 14: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 15: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 16: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s16

Spatial scale: Segment system

www.usda.gov/stream_restoration/chap1.html

Page 17: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 18: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s18

www.usda.gov/stream_restoration/chap1.html

Cross section of a channel

Page 19: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s19

Floodplain

www.usda.gov/stream_restoration/chap1.htmlFigure 1.21

Page 20: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 21: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 22: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 23: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s23

dnr.metrokc.gov/WTD/wetland79/images/oxbow-01-30.jpg

An oxbow lake

Page 24: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

Developed by: Merrick, Richards Updated: August 2003 U1-m4-s24

Spatial scale: Reach system

www.usda.gov/stream_restoration/chap1.html

Page 25: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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

Page 26: Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1

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