River generation pathways (fact sheet 14) Flashcards

1
Q

Another name for water pathways

A

flow paths

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2
Q

Two flow paths that don’t include subsurface flow

A
  1. direct in-channel precipitation

2. infiltration-excess overland flow

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3
Q

Direct in-channel precipitation

A

preciptation falling directly into river channels

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4
Q

Another name of infiltration-excess overland flow

A

Hortonian overland flow (HOF)

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5
Q

Hortonian overland flow/ infiltration-excess overland flow

A

Generated by rainfall intensities greater than the infiltration capacity of the soil

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6
Q

The infiltration capacity is considered to be the permeability of the soil …

A

close to the ground surface

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7
Q

Reasons why HOF isn’t significant

A
  1. soil infiltration capacities are normally seen to be greater than measured rainfall intensities
  2. There are less conerservative ions dissolved in river water than in rain water which suggests than rainfall is stored before discharge into the river
  3. extensive overland flow is rarely observed in catchments
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8
Q

Subsurface stormflow

A

The shallow underground water-pathway that delivers a rainfall response to a river response

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9
Q

Evidence for subsurface response

A

the observation that the rise and fall of a river is matched by a similar rise and fall of a nearby water-table

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10
Q

Three explanations for how subsurface water rapidly moves to the river-side soils

A
  1. shallow water paths
  2. natural soil pipes
  3. wave propagation
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11
Q

Shallow water paths

A

water movement in the top soil

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12
Q

Natural soil pipes

A

tunnels in the soil 1cm to 1m in diameter, formed by waterflow

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13
Q

Wave propagation

A

the input of storm rainfall onto a catchment generates a ‘shock wave’ in the water table that moves much faster than the water movement itself

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