Chapter 5, 6 - Soil water Flashcards
(36 cards)
soil water
water in the soil; a solution, includes nutrients, etc.
atom
smallest unit of an element that retains the properties of the element
molecule
two or more atoms together (H2O)
ionic bonds
attraction between oppositely charged ions
covalent bonds
sharing of electrons between atoms
ion
a charged atom (+ or -)
polar molecule
molecule with unequal charge distribution which creates slightly positive and negative sites on a molecule
hydrogen bonds
H in one molecule will adhere to on O in a different molecule; a weak bond
cohesion
likes adhered to likes (water to water)
adhesion
likes adhered to unlikes (water to solid surfaces, like sand, silt, clay)
surface tension
more attraction of water to water than water to air; water loves to be w/ water; creates a small skin of tension; causes water to boil at ta higher temp than alcohol
capillary movement
movement of water through pores or tubes (capillaries) due to adhesion and cohesion
influences on capillary movement
- pore size (the bigger the size, the slower going up, the faster going down)
- quantity of pores
- distribution of pores (lined up or more random)
kinetic energy
energy being used
potential energy
energy stored, not being used
wet soil potential vs. dry soil potential
wet = high potential; dry = low potential
low because water molecules are held tightly by dry soil, wet soils hold less tightly because it’s already full, so water moves through
soil water potential
the amount of H2O movement that will occur in the soil, how much water can move from one place to another; pure water is baseline for calculation
energy of water is influenced by 3 factors (3 types of water potential)
- gravitational potential
- matric potential
- osmotic potential
gravitational potential
- makes water move
- positive energy potential
- the force of gravity on water
matric potential
- effects of attractive forces betwene water and soil solids (SSC,OM)
- soil solids tend to be a negatively-charged material, so water clings and slows its movement
- always a negative potential, reducing potential energy (water movement)
osmotic potential
- presence and quantity of solutes in the soil water
- solutes in the form of ions (usually)
- reduces movement of water (negative energy, slows it down)
gravitational water
Excess water from rain or irrigation that temporarily fills the macropores, then drains. Considered unavailable to plants.
field capacity
Remaining water after gravitational water has drained away.
permanent wilting point/percentage
When plants are unable to recover at night from daytime wilting. Plant is unable to pull enough water from colloids because it is held too tightly. Remaining water in soil is considered unavailable to plants.