Fluvial Landscapes and Processes

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Flashcards covering key vocabulary and concepts related to fluvial landscapes, hydrology, and sediment transport.

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25 Terms

1
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Channel Head

The upstream boundary of concentrated water flow and sediment transport between definable banks. (Anderson and Anderson, 2010)

<p>The upstream boundary of concentrated water flow and sediment transport between definable banks. (Anderson and Anderson, 2010) </p>
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Catchment Hydrology

The study of how water passes through hillslopes and its interaction with the landscape.(Anderson and Anderson, 2010)

<p>The study of how water passes through hillslopes and its interaction with the landscape.(Anderson and Anderson, 2010)  </p><ul><li><p></p><img src="https://knowt-user-attachments.s3.amazonaws.com/4fdfd08d-d289-4731-bb8c-6ddac56b0a1e.png" data-width="100%" data-align="center"></li></ul><p></p>
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Stream Head

The point where perennial flow occurs in a river system. (Anderson and Anderson, 2010)

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Overland Flow

Water that flows over the ground rather than being absorbed into the soil. (Anderson and Anderson, 2010)

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Groundwater Flow

The flow of water through aquifers, which can be slow and has a unique chemical nature. (Anderson and Anderson, 2010)

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Sediment Transport Modes

The three modes include solution, suspension, and traction, which shape the riverbed. (Anderson and Anderson, 2010)

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Hjulstrom Curve

A graphical representation that indicates the relationship between sediment size and the velocity of water required for erosion or deposition. (Anderson and Anderson, 2010)

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Fluvial Sediment Budgets

The calculation of sediment transport and deposition from catchment areas to global scales, particularly in relation to rainfall. (Anderson and Anderson, 2010)

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Braided River

A river consisting of multiple channels that interweave, often due to excess sediment load. (Anderson and Anderson, 2010)

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Anthropogenic Activities

Human actions that have significant impacts on fluvial landscapes and environmental change. (Lane, 2007)

<p>Human actions that have significant impacts on fluvial landscapes and environmental change. (Lane, 2007) </p><ul><li><p></p><img src="https://knowt-user-attachments.s3.amazonaws.com/33285877-7edb-40d9-9001-032d369ab62c.png" data-width="100%" data-align="center"></li></ul><p></p>
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Process: channel initiation

  • (Anderson and Anderson, 20100

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Types of runoff

  • (Kirkby, 2007)

 

diagram showing timescale of when we might see these flows

<ul><li><p><span>(Kirkby, 2007)</span></p></li></ul><p>&nbsp;</p><img src="https://knowt-user-attachments.s3.amazonaws.com/293c542e-5e53-45b5-98b6-6648057d8429.png" data-width="100%" data-align="center"><p>diagram showing timescale of when we might see these flows </p>
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Occurrence of infiltration-excess overland flow

(Anderson and Anderson, 2010)

 

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Properties of flowing water

(Knighton, 2014)

<p>(Knighton, 2014)</p>
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Continued

<ul><li><p></p><img src="https://knowt-user-attachments.s3.amazonaws.com/63504b5d-2601-4617-9621-28115b6fb6ba.png" data-width="100%" data-align="center"></li></ul><p></p>
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Transportation

  • (Knighton, 2014)

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Measuring river flows

  • Knighton, 2014 - for the picture

<ul><li><p><span>Knighton, 2014 - for the picture </span></p><img src="https://knowt-user-attachments.s3.amazonaws.com/940f70c8-e558-48ea-befe-aa2b32b8ebbf.png" data-width="100%" data-align="center"></li></ul><p></p>
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Gauging a river with a cross-section

Measures how fast a river is going - Knighton, 2014

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Weirs and Flumes

Funnel rivers into a structure so it can be measured more easily - Knighton, 2014

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Acoustic Doppler current profiler

Scans river bed, covers the whole cross-section - Knighton, 2014

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Fluvial sediment budgets: catchment to a global scale

  • Knighton, 2014

<ul><li><p><span>Knighton, 2014 </span></p><img src="https://knowt-user-attachments.s3.amazonaws.com/0348499d-28ef-4ce5-bc1e-99bf9b7e8c9f.png" data-width="100%" data-align="center"></li></ul><p></p>
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Sediment delivery to streams by landslides during earthquakes

knowt flashcard image
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River response to landslides

types of events that are responsible for high sediment flux

the way sediment is delivered to oceans is not stable

<p>types of events that are responsible for high sediment flux </p><p>the way sediment is delivered to oceans is not stable </p>
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Channel platform

  • Knighton, 2014

 

 

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Case study: Peace River Canada

  • Knighton, 2014