Ch 9 Flashcards
(39 cards)
Outgassing:
Water deep in the interior of the earth (below crust), are released in the form of gas (vapors)
Eustasy:
global sea level caused by changes in the volume of water in the oceans
In a globe, where is mostly water and where is mostly land
Land is mostly found in the northern hemisphere, water in the southern hemisphere
The hydrological cycle
Vast currents of water, water vapor, ice, and associated energy
3 components:
1- atmosphere
2- surface
3- subsurface
What happens in
the atmosphere part?
Evaporation + transpiration = evapotranspiration
transpiration: when plants release water to the atmosphere through small openings called stomata in their leaves, which is another way water moves into the atmosphere from land environments including water moving from the soil into plant roots and passing through their leaves to the air
What happens in the surface?
Interception
stemflow
through fall
what happens in the subsurface?
infiltration
Overland flow
surface run off
percolation
Infiltration:
Water get soaked by the soil
What happens if the ground surface is permeable?
then it won’t soak up the water
surface run off:
Same as overland flow
Overland flow
Surplus of water on surface so it causes a runoff in an area
Percolation:
the movement of water through rocks and soil, filtering downwards after it has infiltrated the ground
Soil-moisture zone
area where most of the water is stored in the soil, and roots have access to it
Zone of saturation
When soil is fully saturated, extra water moves downward as gravitational water into deeper groundwater, filling all spaces in the soil
Base flow
when water table reaches a stream, groundwater flows into the stream
describe the water budget:
measures the input of precipitation and its outputs like evapotranspiration, evaporation, and transpiration from plants, and surface runoffs, and moisture in the soil moisture zone.
income = precipitation
expenditure = run off, evaporation, transpiration
savings account = soil moisture storage
Rain gauge:
measures the amount of precipitation, its like a big cup that collects all of it
Potential evapotranspiration:
the amount of water that would evaporate and transpire if there was always enough water available
Actual evapotranspiration:
the water deficit, the subtraction of the water deficit by the (PE)
3 categories of water:
gravitational: drains downwards after filling the soil pore spaces
hygroscopic and capillary:
Both remain in the soil but ONLY capillary is accessible to plants image below
Why is hygroscopic water not accessible to plants?
it is a thin molecule layer tightly bound to each soil particle by the hydrogen bonding of water molecules
Wilting point of a plant:
when soil moisture only contains inaccessible water, so plants wilt and die
Capillary water:
valid for plants
Gravitational water:
un valid for plants as it percolates deep to the groundwater zone