Chapter 3 Flashcards
lentic
standing water
lotic
flowing water
ephemeral
formed after a rainfall, then disappears
intermittent
flows for a while but then dries up
perennial
stays flowing all year during normal rainfall patterns
what shapes a river?
- climate
- geology
- topography
- vegetation
- human use
colluvial
organic matter that gathers at the bottom of hill slopes
alluvial
sediment and organic matter that is carried down from upstream
stream network organization
heirarchical
- headwaters are erosional
- medium order streams transfer sediments
- higher orders are depositional
spatial framework
- longitudinal dimensions
- lateral connectivity
- vertical connectivity
stenotherm
narrow temperature range
eurytherm
large temperature range
water balance
preciptation+ground water= discharge+ evapotranspiration + ground water out
(ppt=Q + ET)
discharge
flow (Q), volume of water flowing through a cross sectional area of a stream per unit time, Q = AxV
thalweg
deepest part of the channel
factors influencing flow
- slope (gravity)
- cross-sectional area
- roughness of bottom
- wetted perimeter
wetted perimeter
boundary between stream water and sediment
laminar flow
fluid movement in smooth, regular layers with no dusruption between layers. Adjacent layers slide by one another, occurs at low velocities
turbulent flow
fluid movement is irregular, mixing