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1. How does water movethrough the drainage basin system?
2. Elements of a drainage basin: Inputs Flow / Transfer Storage
Output
3. Input: major input - precipitation. The type: rain or snow,
hail, etc. Factors affecting the amount of water in the system: the
intensity, the duration and Frequency of the precipitation
5. Interception defined as the capture of precipitation by the
plant canopy and return to the atmosphere through evaporation or
sublimation.* Interception loss: water which is retained by plant
surfaces and which is later evaporated away & absorbed by
plant
6. leaf type increase interception capacity if leaves &
twigs are dry wind speed the higher the wind speed the lower the
interception capacity - the more frequent the storm events lesser
the interception loss temperature, and the humidity of the
atmosphere
7. Throughfall: the process of precipitation passing through
the plant canopy (Yellow lines) Factors affecting: plant leaf and
stem density, type of the precipitation, intensity of the
precipitation, and duration of the precipitation event.
8. Stemflow: is the process that directs precipitation down
plant branches and stems (red arrows ). this process causes the
ground area around the plants stem to receive additional moisture.
The amount of stemflow is determined by leaf shape and stem branch
architecture. In general, deciduous trees have more stemflow than
coniferous vegetation.
9. Infiltration Some of the precipitation seeps into the ground
and stored in aquifers then it is transported to streams and lakes
by subsurface flow. The amount of infiltration is influenced by:
the permeability and moisture content of the soil, the presence of
vegetation and the volume and intensity of
10. Overland Flow Rills - Water moving over ground in small
channels Sheetflow - Water moving over ground across the whole
surface Hortonian Overland Flow: Saturated Overland Flow:
infiltration excess overland Long period of steady flow rain and
water table reach the surface rainfall is greater than infiltration
capacity No additional water can E.g. If a soil surface can be
infitrated so must infiltrate 30mm/hr but remain on surface
precipitation is 40mm/hr, therefore 10mm will be overland flow
Common in the temperate Very common in the tropics
11. Overland flow
12. Rills
13. Sheetflow
14. A process where water enters the ground vertically through
pores Factors affecting infiltration: Intensity & duration of
the precipitation Type of soil Vegetation & Land cover Slope of
the land Evapotranspiration Soil saturation
15. the slow movement of water through compact layers of soil
and rocks Factors affecting percolation: Precipitation Relief
steeper the gradient the less water will be percolated Flora &
fauna animal tunnels & burrow - root system of direct movement
of water in the soil Rock structure / composition Porous rock
sandstone Permeable rock - limestone
16. Water transfers laterally in the aquifers If the water
table reaches the surface it means ground is saturated.(a)
infiltration to deep groundwater,(e) overland flow to (g)(g)
temporary ponds(f) deep groundwater flow.
17. Channel flow Water transfers to channel through 3
processes: Surface run-off Throughflow Groundwater flow
/baseflow
18. Rainfall Vegetation and land use Climate Shape Conditions
in drainage basin Size and shape of the river basin Soil type and
depth Bedrock
20. Process of percolation produces groundwater storage Water
collected above the impermeable layer Or it may fill all the pores
spaces, creating a zone of saturation Above the impermeable layer,
there are 3 zones: An unsaturated zone A saturated zone An
intermediate zone
21. Soil pores are mostly filled with microchannels so water
can move as percolation and throughflow Biological activity with
plant roots, soil flora and fauna create microchannels
22. Water accumulates all the soil pores are full of water
Baseflow / groundwater occurs No biological activity
23. Zone between the unsaturated and saturated zones Changing
patterns of precipitation and EVT throughout the year gives a layer
which is alternatively saturated and unsaturated Interflow
occurs
24. 18 Infiltration rate 16 Rainwater which is not infiltrated
will become 14 surface run-off / overlandInfiltration Rate flow 12
10 8 6 4 2 0 1 2 3 4 5 6 Hours from the start of rainfall