ENVS 3060

    Cards (25)

    • Groundwater (GW):
      • Is water stored in cracks in soil, sand and rock
      • Often below water table
      • Generally in saturated conditions
    • GW Problems:
      • Misuses - waste, overuse
      • Contamination
      • Knowledge gap, user awareness
    • Aquifer: underground water body
    • Soil Water (SW):
      • Stored in soil pores (void space)
      • Above water table
    • Wet Bulk Density
      Pw=Pw =Mt/Vt Mt / Vt
    • Dry Bulk Density
      Pb=Pb =Ms/Vt Ms / Vt
    • Particle Density
      Pp=Pp =Ms/Vs Ms / Vs
    • Gravimetric Water Content
      θw=θw =Mw/Ms Mw / Ms
    • Volumetric Water Content
      θw=θw =Vw/Vt Vw / Vt
    • θv=θv =θwPb θw Pb
    • Density of water = 1gcm^-3
    • Porosity:
      • how porous the soil is
      • pores can be filled with liquid or air
    • Void Ratio
      e=e =Vair+ Vair +Vwater/Vsolids Vwater / Vsolids
      void ratio = empty space / solid space
    • Water Filled Porosity
      fw=fw =Vw/Vt= Vw / Vt =θv θv
    • Air Filled Porosity
      fa=fa =Vair/Vtotal= Vair / Vtotal =fθv f - θv
    • Total Porosity
      f=f =Vf/Vt Vf / Vt
    • Saturation Ratio
      θs=θs =θv/f θv / f
    • Porosity Factors
      • Packing
      • Grain shape
      • Grain size
      • Sorting
      • Grain orientation
    • Macropore > Mesopore > Micropore
    • Saturated: all water below water table (groundwater)
    • Cohesion: attraction of water molecules to each other
    • Adhesion: attraction of water molecules from solid surfaces
    • Surface Tension: force of attraction between the water molecules on the surface
      Sphere drop of water is caused by pressure from air (balancing of pressure)
    • Capillary Action: movement of water through soil pores due to adhesion, cohesion, and gravity
    • Soil is just a bunch of capillaries (a capillary system)
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