soil physics: Infiltration & evaporation Flashcards
what are the 4 types of pores in the soil, what are they a function of, and how do they affect conductivity
macro and micropores describe size, related to texture. macropores release water rapidly = rapid conductivity and the inverse for micro
continuous and noncontinuous (noncontinuous pores caused by compaction) which reduces conductivity
what is the saturated hydraulic conductivity, what is high conductivity, and what is the measurement
this measures how fast the water moves in soil, this relates to the type of pores. high conductivity is when pores are large enough for water and air and are continuous
Ksat or mm/day
how will management be affected by a soil with high Available water capacity and high hydraulic conductivity
this means soil can store a lot of water however it will drain quickly therefore irrigators need to apply constant water however in small amounts
what is darcys law
-(Q/A) = -ks * (H + L/L)
the flow rate of water in soil is a function of potential difference and conductivity
when does runoff occur from a conductivity perspective
when the application eg rainwater irrigation, exceeds the infiltration rate
how does erosion occur through runoff (3 ways)
- splash impact (little)
- sheet (soil moves as a sheet)
- rill (water moves over weak point)
depends on slope and cover
how do you measure the hydraulic conductivity in the field
constant head permeameter, measure infiltration per minute, estimate using the slope of the flat line (not rapid flow)
what happens when there is no potential difference
no movement will occur
what happens when there are different texture layers in the soil profile (Ksat)
subsurface lateral flow due to difference in hydraulic conductivity cannot penetrate layer beneath then there will be evaportation, slow penetration or if on hill more lateral flow
what is the water pressure in darcys law
height of water above the soil
what is the wetting front
the interspace between the unchanged soil and the saturated zone after infiltration.
what is the short term infiltration rate
water moves rapidly into the soil controlled by sorptivity, texture and moisture content
what is the long term infiltration rate
water moves steadily due to hydraulic conductivity structure and texture
what is slaking
in soils with low OM that cannot hold aggregates together, moisture will rapidly infiltrate aggregate and it will break due to pressure
what is the effect of slaking after the water is dried
if on topsoil a crust can form which reduces infiltration and seedling emergence, some particles will settle and create a compact subsurface