Lecture 7 - Atmosphere-Plant-Soil Continuum Flashcards
osmosis
water uptake from soil to roots
what does soil particle size affect
water movement
water retention
how does water movement in large pore space vs small pore space in soil differ
large pore space - more gravitational pull (moves down faster)
small pore space - more capillary action (spreads out and down at a slower pace
saturation
all pores are full of water. gravitational water is lost
field capacity
available water for plant growth
wilting point
no more water is available to plants
what other factors affect soil interactions with water
organic matter, microbes, salinity, etc.
root architecture
length of roots, branching, angle
what is root architecture affected by
water flow into roots
what are shallow root systems effective at
catching limited rainfall
hydrotropism
root growth in response to water deficit
examples of hydrotropism on root growth
in water sufficient environments, gravity makes the root grow down
in water insufficient conditions, root will grow towards water against gravity
root pressure
positive pressure that forms in the roots as the roots uptake water from the soil via osmosis
guttation
happens in the early morning when transpiration is not very high, Roots push water up and they need to release some water through the hydathode, forming water droplets on leaves
different types of water pathways
apoplasmic, symplasmic, and transcellular