Lecture 9 soil water Flashcards
what is matric potential dependent on
pore geometry
por size distribution
particle aggregation
soil water content
what can field capacity be dependent on
wetting history (can become hydrophobic) soil type OM content depth of wetting plant uptake pattern
definition of PMP
permanenet wilting point, water content of soil so low that even if ET =0 plants cant take up
when can wilting occur
et rate exceeds uptake
no water
too salty for osmotic potential
three ways to measure infiltration
ring infiltrometer
furrow infiltrometer
sprinkling infiltrometer
whats the effect of rewetting on infiltration rates
infiltration rates drop when rewetting, because soil structure tightens before rewetting due to the negative pore pressures
what are the four stages for the inflow hydrograph
advance stage (water getting to end of field)
soaking stage
depletion
recession (top of field goes dry)