Topic 3: Soil Water Flashcards
SMAP
soil moisture active passive
Phreatic Zone
zone of saturation (realm of groundwater )
water table
maximum height of groundwater , level which below ground is saturated with water
capillary fringe
subsurface layer in which groundwater seeps up from a water table by capillary action to fill pores
Vadose Zone
unsaturated zone, realm of soil moisture
what is the structure of soil?
45% mineral particles 25% air 25% water 5% organic matter *water and organic content can vary
properties of clay
highly weathered particles
mostly clay minerals
adsorbs soil water very effectively
adsorption
water in surface layer stuck through electromagnetic forces
properties of sand/silt
less weathered particles
less reactive/charged
retain less soil water
larger pores, higher hydraulic conductivity
less total pore volume= more or less porosity?
less porosity
list some soil properties
- grain size and type
- -sorting
- -bulk density
- -water content, degree of saturation
- -hydraulic conductivity
- -thermal state
main components of soil by mass
solid and water mass ((Mm and Mw)
main components of soil by volume
mineral, water and air (Vm, Vw, Va)
what is volumetric water content
fraction of water in soil, amount of pore space filled with water. at saturation Va=0
adsorbed/hygroscopic water vs. capillary water vs. gravitational water
capillary is least tightly held between grains, hygroscopic is right around the soil particle and is the most tightly held. gravitational water is the air or space otherwise impacted by gravity.
what is field capacity
water in soil that can be retained against gravity from adsorbed water and capillary pressure
what is permanent wilting point
is the water content at which plants cannot draw water out of the soil
what is available water
water that is available to plants
what is gravimetric water content?
is the mass fraction of water in the soil
what is gravitational water?
water in a soil that is freely available for gravitational drainage (free water in pore space)
divisions of the subsurface P water vs P atmos
Vadose Zone: PwP atmos
what is surface tension
is a function of the interaction between the two materials at the interface
does suction increase or decrease with increased pore size?
decreases with larger pore diameter
what is suction a function of?
moisture content and where it is wetting/drying
which pores fill first ? when drying, which pores empty first?
wetting: small pores fill first so water increases slowly
drying: large pores empty first, rapid decline in water
hydraulic conductivity at high vs low water contents
high water contents: coarse soils have a higher hydraulic conductivity than fine soils
low water contents: fine soils have a higher hydraulic conductivity than course soils
how do plant stake up water from the soil?
through osmosis
how much soil water is used for photosynthesis vs waste
1-2% for photosynthesis and tissue growth, 98% waste
how is excess water evacuated from a plant
opening of the stomata, occurs during the day, downfall is only a 1:600 ratio of CO2 to H2O
does water move faster or slower in saturated soil?
it moves faster- 1-10cm/hr vs. unsaturated at 1mm/hr
forces that draw water up
osmotic pump pulling water into plant roots (overnight)
evapotranspiration (daytime)