Lecture 4: Hydrology Flashcards
What processes form soil structure
biological, physical, bio-physical
Size of pores in healthy soil
more than solids
bulk density
low: pores>solids
high: solids>pores (compacted)
bulk density calculation
mass of soil/volume of soil
soil texture interacts with bulk density
higher bulk density is more energetically-costly for plants
catchment (watershed)
landscape that behaves as a discrete hydrological unit
water cycle (rainfall intercepted by vegetation)
precipitation excess drips onto ground
infiltration
overland flow (water on top of land)
interflow (moving water inside soil)
baseflow (water moving in groundwater)
water cycle (water in plants)
photosynthesis
transpiration
evaporation of soil water
albedo potential
evaporation of soil water when sunny
higher in grass and croplands than forests
types of pores
water storage pores (innaccessible to plants)
transmission pores (network between aggregates)
transmission pores
plants get nutrients and water from mass flow
mass flow
movement of nutrient dissolved in solution as water absorbed for transpiration
saturated soil shave different types of water
hygroscopic: adheres to soil particles
capillary: micropores hold water so plants can access
gravitationsal: drains out of root zone
wilting point
water left that adheres to soil particles
water holding capacity
interaction between soil texture and pore space
water available to plants