Hydrology and Fluvial Geomorphology: River channel processes and landforms Flashcards

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1
Q

What is hydraulic action?

A

Sheer power/force due to the water’s velocity which allows joints and cracks to be exploited, leading to the fragmentation of the rock and the dislodging of particles (may also contribute to cavitation)

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2
Q

Cavitation

A

The force of air exploding. As fluids accelerate, pressure drops and air bubbles may form. Cavitation is the implosion of these trapped air bubbles, a process which evicts tiny jets of water with velocities of up to 130 km/h, which can weaken solid rock.

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3
Q

Attrition

A

Load particles knock against each other and are worn away, becoming smaller and rounder.

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4
Q

Corrosion/solution

A

A chemical action which dissolves chemical ions in carbonate rocks such as limestone.

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5
Q

Abrasion/corrasion

A

The erosion/wearing away of the channel banks and bed by coarse and angular fragments of hard rock carried within the river’s lad. These particles are thrown against the bed and banks by fast-flowing river flow and are used as a mechanical tool for grinding them. This may produce pot holes where pebbles become trapped in the bed and are whirled around by the current. It is assisted by turbulent flow where the speed of the water is continuously undergoing changes in magnitude and direction

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6
Q

Traction

A

Larger, coarser load ar rolled along the stream bed by the river current

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7
Q

Saltation

A

The hopping or bouncing motion of medium-sized particles along the bed of the river as a result of sufficient river energy

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8
Q

Suspension

A

Light sediments are suspended above the bed by the current and moved within the body of the water

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9
Q

Solution

A

The transport of soluble material dissolved in the river water

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10
Q

Competence

A

Maximum particle size that a river can transport

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11
Q

Capacity

A

Maximum load that a river can transport

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12
Q

Which factors affect rate of erosion? (9)

A

Discharge, human impacts, velocity, competence, type of rock, pH, load, vegetation, relief

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13
Q

When do river deposit their load?

A

When they slow down. When gradient becomes more shallow. When volume decreases. When friction increases.

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14
Q

Deposition

A

When the river loses its energy so it is forced to drop its load (heaviest first)

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15
Q

Sedimentation

A

The deposition of sediment

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16
Q

Important features of the Hjulstrom curve (3)

A
  1. Smallest and largest particles require high velocities to lift them - clay resists entrainment due to its cohesion
  2. Higher velocities are required for entrainment than for transport
  3. When velocity falls below a certain level, those particles are deposited
17
Q

Three types of flow

A

Laminar, turbulent, helicoidal

18
Q

Three channel types

A

Straight, braiding, meandering

19
Q

Thalweg

A

Path of quickest flow