Stream Ecology: River Structure and Hydrology Unit 1: Module 4, Lectures 1 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-s2 Module 4 introduces students to: Lecture1: Lecture 2: The Importance of Rivers The Hydrologic Cycle Watersheds as a concept Geomorphology Hydrology flow and discharge storm and annual hydrographs flood probability sediment transport and deposition watersheds and drainage networks channel morphology habitat scales Developed by: Merrick, Richards Updated: August 2003 U1-m4-s3 Importance of rivers Rivers: Provide Provide Provide Provide Provide water and nutrients for agriculture habitat to diverse flora and fauna routes for commerce recreation electricity www.aquatic.uoguelph.ca/rivers/chintro.htm Developed by: Merrick, Richards Updated: August 2003 U1-m4-s4 Natural watercourses Existence depends on: Availability of surface water A channel in the ground An inclined surface www.aquatic.uoguelph.ca/rivers/chintro.htm Developed by: Merrick, Richards Updated: August 2003 U1-m4-s5 Lotic systems Four dimensions: Longitudinal Lateral Vertical Time www.aquatic.uoguelph.ca/rivers/chintro.htm The four dimensions of a lotic system Developed by: Merrick, Richards Updated: August 2003 U1-m4-s6 Variation in time and space 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 Developed by: Merrick, Richards Updated: August 2003 U1-m4-s7 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-s8 The hydrologic cycle ga.water.usgs.gov/edu/charts/waterdistribution.gif Developed by: Merrick, Richards Updated: August 2003 U1-m4-s9 Distribution of water on earth ga.water.usgs.gov/edu/charts/waterdistribution.gif Developed by: Merrick, Richards Updated: August 2003 U1-m4-s10 What is a watershed? www.dec.state.ny.us/website/2000/watersheds.gif Developed by: Merrick, Richards Updated: August 2003 U1-m4-s11 What is a watershed? www.dec.state.ny.us/website/2000/watersheds.gif www.aquatic.uoguelph.ca/rivers/chwater.htm Developed by: Merrick, Richards www.epa.gov/watertrain/ecology/ecology21.html Updated: August 2003 U1-m4-s12 Spatial scale: Stream segments www.usda.gov/stream_restoration/chap1.html Developed by: Merrick, Richards Updated: August 2003 U1-m4-s13 Stream networks or drainages www.usda.gov/stream_restoration/chap1.html www.aquatic.uoguelph.ca/rivers/chwater.htm Developed by: Merrick, Richards Updated: August 2003 U1-m4-s14 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-s15 Spatial scale: Segment system www.usda.gov/stream_restoration/chap1.html Developed by: Merrick, Richards Updated: August 2003 U1-m4-s16 Stream corridor and channel morphology http://www.usda.gov/stream_restoration/Images/scrhimage/chap1/fig1-15.jpg Developed by: Merrick, Richards Updated: August 2003 U1-m4-s17 Cross section of a channel www.usda.gov/stream_restoration/chap1.html Developed by: Merrick, Richards Updated: August 2003 U1-m4-s18 Floodplain www.usda.gov/stream_restoration/chap1.html Figure 1.21 Developed by: Merrick, Richards Updated: August 2003 U1-m4-s19 Meandering rivers A meander becomes more pronounced as the streamline shifts between the river banks. Developed by: Merrick, Richards Formation of an oxbow lake http://www.aquatic.uoguelph.ca/rivers/chphys.htm Updated: August 2003 U1-m4-s20 Sinuosity: Gradient and substrate Big meanders low gradient fine substrates Developed by: Merrick, Richards Small meanders high gradient coarse substrates Updated: August 2003 U1-m4-s21 Braided channel Braided Pattern = high slope + high stream power + coarse bed materials earthsci.org/teacher/basicgeol/stream/stream.html#Erosion%20by%20Streams Developed by: Merrick, Richards Updated: August 2003 U1-m4-s22 An oxbow lake dnr.metrokc.gov/WTD/wetland79/images/oxbow-01-30.jpg Developed by: Merrick, Richards Updated: August 2003 U1-m4-s23 Spatial scale: Reach system www.usda.gov/stream_restoration/chap1.html Developed by: Merrick, Richards Updated: August 2003 U1-m4-s24 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-s25 Pool - riffle sequence Riffle to riffle = 5 - 7 channel widths http://www.usda.gov/stream_restoration/Images/scrhimage/chap1/fig1-15.jpg Developed by: Merrick, Richards Updated: August 2003 U1-m4-s26