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Streams and Rivers

Hydrology Stream Processes

TermDefinition
Hydrosphere the Earth's water - 71% of the Earth's surface is covered with oceans and seas
Terrestrial (rocky) Planets Mercury, Venus, Earth, and Mars
Hydrologic Cycle the source of all freshwater on land, and the natural recycling of water
How the Hydrologic Cycle works: - water evaporates from oceans -released water vapor is transpiration - vapor condenses and precipitates - 20% of precipitation falls on land - some water runs off back to bodies of water, some stay on land in river, streams, or glaciers, etc.
Laminar Flow little mixing takes place between adjacent flow lines within the fluid
Turbulent Flow the lines of flow are complexly intertwined
Runoff occurs when rainfall intensity exceeds the infiltration capacity of the soil
If rainfall is ABSORBED... there is no runoff
When the ground is SATURATED... runoff begins
Sheet Flow the water moves as a continuous film of water flowing over the surface. Sheet flow is not confined and is common on hard flat surfaces.
Channel Flow the surface runoff is confined in a channel, which is a trough-like depression
Gradient When water flows downhill over a slope
Velocity of running water measure of the distance water travels in a given amount of time
Discharge the volume of water that passes a given point in a given amount of time
Measuring the discharge of a waterway = Channel width × channel height × stream velocity
Tributary small stream running into a larger river
Hydraulic Action the impact of water, which is quite effective in dislodging loose soil and sediment
Abrasion occurs when running water carries sand and gravel that wear away any rock surface they move over
Dissolved Load invisible because it is composed of ions which are transported in solution
Suspended Load made up of the smallest particles that can be kept in suspension in the water by turbulence
Bed Load composed of sand and gravel that is transported along a stream’s bed by saltation, rolling, and sliding
Alluvium sediment deposits of running water
Braided Streams have too much sand and gravel to effectively transport, so the sand and gravel are deposited as bars that divide the main channel into many channels
Meandering Streams carry much more suspended load and have a single, sinuous channel
Created by: user1115
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