ch10 flashcards
(65 cards)
hydrologic cycle
The continuous movement of water on, above, and below Earth’s surface through processes like evaporation, condensation, precipitation, infiltration, and runoff
overland flow
Water flowing over the land’s surface before entering a stream channel; occurs as sheetflow (thin layers) or rivulet flow (small, concentrated channels)
sheetflow
A thin, uniform layer of water moving over the ground surface, typically formed after rainfall before water collects into channels
rivulet flow
Overland flow that becomes concentrated into small channels or rivulets, often leading to the formation of stream channels
stream discharge (Q=AV)
The volume of water flowing past a point in a channel per unit time, calculated as the product of cross-sectional area (A) and velocity (V)
flood hydrograph
A graph showing how a stream’s discharge changes over time during and after a precipitation event, illustrating lagtime and peak discharge
lagtime
The time delay between peak rainfall and peak stream discharge, influenced by factors like vegetation, soil permeability, and urbanization
valley enlargement
The process by which stream valleys grow larger over time through downcutting (deepening), headward erosion (lengthening upstream), and widening of valley walls
downcutting
The process by which a stream erodes its channel bed, deepening the valley and lowering its base level
headward erosion
The upstream extension of a stream channel by erosion at its head, capturing new drainage areas and lengthening the stream
widening
The lateral erosion of stream banks that broadens the valley, often caused by increased meandering and undercutting
stream erosion
The removal of rock and soil by moving water, primarily through hydraulic action, abrasion, and solution
hydraulic action
The erosive force of moving water as it exerts pressure, lifts and removes loose sediments, and enlarges cracks in rock
abrasion (in streams)
Erosion caused by the grinding action of sediment and rock fragments carried by the stream acting like sandpaper on the channel bed and walls
dissolved load
The portion of a stream’s load composed of soluble minerals dissolved in the water
suspended load
Fine sediment (clay, silt, and fine sand) carried in suspension by the turbulence of the water, giving the stream a muddy appearance
bed load
Coarser particles (sand, gravel, pebbles) that move along the stream bed by rolling, sliding, or hopping (saltation)
competency
A measure of the largest particle size a stream can transport; increases with velocity and discharge
capacity
The total amount of sediment a stream can carry, depending on its discharge and velocity
stream velocity
The speed of water flow in a channel, influenced by gradient, channel shape, sediment load, and water volume
stream gradient
The slope or steepness of a stream channel, generally decreasing downstream and affecting flow velocity and erosion
channel shape
The geometry (width, depth, roughness) of a stream’s channel, influencing flow resistance, velocity, and sediment transport
sediment load
The total amount of sediment (dissolved, suspended, and bed load) carried by a stream at any given time
water volume
The amount of water in a stream (discharge), impacting its ability to erode, transport sediment, and shape the landscape