River generation pathways (fact sheet 14) Flashcards
Another name for water pathways
flow paths
Two flow paths that don’t include subsurface flow
- direct in-channel precipitation
2. infiltration-excess overland flow
Direct in-channel precipitation
preciptation falling directly into river channels
Another name of infiltration-excess overland flow
Hortonian overland flow (HOF)
Hortonian overland flow/ infiltration-excess overland flow
Generated by rainfall intensities greater than the infiltration capacity of the soil
The infiltration capacity is considered to be the permeability of the soil …
close to the ground surface
Reasons why HOF isn’t significant
- soil infiltration capacities are normally seen to be greater than measured rainfall intensities
- There are less conerservative ions dissolved in river water than in rain water which suggests than rainfall is stored before discharge into the river
- extensive overland flow is rarely observed in catchments
Subsurface stormflow
The shallow underground water-pathway that delivers a rainfall response to a river response
Evidence for subsurface response
the observation that the rise and fall of a river is matched by a similar rise and fall of a nearby water-table
Three explanations for how subsurface water rapidly moves to the river-side soils
- shallow water paths
- natural soil pipes
- wave propagation
Shallow water paths
water movement in the top soil
Natural soil pipes
tunnels in the soil 1cm to 1m in diameter, formed by waterflow
Wave propagation
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