Hydrology and Fluvial Geomorphology Flashcards
open system
allows the movement of energy and matter across its boundaries
precipitation
conversion and transfer of moisture in the atmsophere to the land
snow/hail/rain/frost/dew
stores
vegetation surface soil moisture groundwater water channels
characteristics that affect local hydrology
total amount of precipitation intensity type geographical distribution variability
interception
interception loss
throughfall
stemflow
evaporation
process by whcih a liquid or solid is changed into a gas
factors affecting evaporation
albedo temperature wind speeds humidity vegetation cover
transpiration
evaporation + transpiration
water vapour escapes from a living plant
potential evapotranspiration
potential evapotranspiration is the water loss that would occur if there was an unlimited supply of water in the soil for use by the vegetation
infiltration
water soaks into or is absorbed by soil
infiltration capacity
the maximum rate at which rain can be absorbed by a soil in a given condition
factors affecting infiltration
duration of rainfall antecedent soil moisture soil porosity vegetation cover raindrop size slope angle
percolation
when water moves slowly downwards from the soil into the bedrock
phreatic zone
permanently saturated zone within solid rocks and sediments is known as the phreatic zone
aeration zone
seasonally wetted and dried zone
baseflow
part of a rivers discharge provided by groundwater seeping into the river
aquifers
permeable rocks (ie. sandstone and limestone) that contain significant quantities of water
flow of a river is influenced by
amount and nature of precipitation local rocks' porosity and permeability shape (morphology), slope and area of the drainage basin amount and type of vegetation cover amount and type of soil cover climate
flood hydrograph
shows how the discharge of a river varies over a short time
time lag
time between the height of the storm and the maximum flow
peak flow
maximum discharge of the river
factors affecting storm hydrographs
precipitation type and intensity temperature and evapotranspiration antecedent moisture drainage basin size and shape drainage density porosity and impermeability of rocks and soils slopes vegetation type land use
critical erosion velocity
lowest velocity at which grains of a given size can be moved
competence
diameter of the largest particle that can be carried
reasons for deposition
a shallowing of gradient which decreases velocity and energy
decrease in the volume of water in the channel
increase in the friction between water and channel
abrasion (corrasion)
wearing away of the bed and bank by the load carried by the river
depends on the concentration, hardness and energy of the impacting particles and the resistance of the bedrock
attrition
wearing away of load carried by river
creates smaller, rounder particles
hyrdraulic action
force of air and water on the sides of rivers and in cracks includes cavitation (force of air exploding)
solution (corrosion)
removal of chemical ions
affected by bedrock, solute concentration, discharge and velocity
factors affecting erosion
load
velocity
gradient
geology (softer rocks easier to erode)
pH (corrosion faster when water is more acidic)
human impact (deforestation, dams and bridges increase rate of erosion)
Manning’s Equation
Q = (AR^2/3 x S^1/2) / n
if bed roughness increases, velocity and discharge decrease
Flows (3)
Laminar
Turbulent
Helicoidal
Laminar Flow
smooth, straight channel with a low velocity
water flows in sheets parallel to the channel bed
Turbulent Flow
higher velocities and features such as meanders
causes variations in pressure within the water
associated with hydraulic action
-> vertical turbulence may create potholes
Helicoidal Flow
aka Horizontal turbulence
corkscrewing motion
Sinuosity
length of a stream channel expressed as a ratio of the valley length
Thalweg
line of maximum velocity
Pools
Fine sediment deposited at low velocity by Eddies in turbulent water
Riffles
Coarse sediment deposited at high velocity by Eddies in turbulent water
Floatation
twigs and leaves
Traction
rolling, discharge high, big objects ie rocks
Saltation
bouncing, small sediment
Suspension
suspended in the water
Solution
dissolved in the water