module 3 Flashcards
precipitation
moisture falling from air -snow water
interception
Water being prevented from reaching the surface by trees or grass
Infiltration
reaches soil moves down into ground
Runoff
water that flows over the ground surface rather than soaking into the ground
ground water
water entering soil seeps down layer of clay or rock
Transpiration
evaporation of water from internal surface of leaves, stems and other living parts
evaporation
liquid to gas
Evapotranspiration
total amount of evaporation of water surfaces of ground and vegetation
properties of water polar- latent heat density relationship with temp cohesion viscosity buoyancy
polar
high specific heat-high resistance to temp
latent heat-energy required to change from one substance to the other
density- inverse relationship with temp
cohesion-stick together-surface tension
viscosity- aquatic vertebrates streamlined
buoyancy- reduces effects of gravity- organisms large
density and temp relationship of water
inverse relationship
water is most dense at
4 degrees celsius
ice floats
longer wavelengths
go deeper at a higher rate, absorbed very quickly
shorter wavelengths
scatter as they move through the water
sunlight and warmth of water
decline in temp with depth
thermocline
layer of water where temperature changes rapidly with depth from warm to cold
temperature produces zonation in any water
epilimnion-upper layer, warm less dense
thermocline- rapidly changing temp prevents mixing
hypolimnion- lower layer, cold more dense
tropics vs. temperate zones thermocline
Tropics Thermocline is permanent surface water is always warmer
Temperate zone Summer Thermocline is present Surface water is warmest
Temperate zone(fall)
Fall surface water begins to cool cool water sinks warmer water moves to the surface, also cools eventually temperature becomes uniform
Turnover
layer at the top move down
Vertical mixing
Moves nutrient
what is a Stream or river
Flowing body of water
Temperature Variable warm and cool, depending on the season shaded areas are cooler than those exposed to sunlight
Temperature affects stream community structure
cool water versus warm water organisms
Solubility of oxygen in water
-with temp increase
with pressure increase
with salinity increase
A function of:
solubilityDecreases as temperature increases
solubilityIncreases as atmospheric pressure increases
Solubility decreases as salinity increases
Oxygen is lost through
uptake by aquatic organisms
increased water temperature
Oxygen is highest at the and lowest at the
Highest at the surface Diffusion Photosynthesis
Lower with increasing depth cellular respiration
Turnover and oxygen in the deep
As warm and cold waters rise and fall Deeper water is recharged with oxygen
What happens in the winter? with oxygen
oxygen demand is what
what does ice do?
oxygen solubility is higher at lower temperatures
oxygen demand reduced for most organisms
Ice reduces diffusion from the atmosphere
pH range of natural waters
acidic
seawater ph
alkaline
limestone vs. granite
watersheds dominated by limestone (CaCO3) higher pH and well-buffered
watersheds dominated by sandstone or granite lower pH, less well-buffered